text:
Russell Baze

Russell Avery Baze (born 7 August 1958 ) is a retired horse racing jockey. He holds the record for the most race wins in North American horse racing history, and is a member of the United States Racing Hall of Fame and the State of Washington Sports Hall of Fame.

Family background
Born to an American family, Baze's father, Joe Baze, is a former jockey and trainer who was competing at Exhibition Park in Vancouver at the time of his birth giving him dual Canadian/American citizenship.

Riding career
Baze began his racing career in Walla Walla, Washington in 1974 and won his first race that fall at the Yakima racetrack. By the early 1980s he was making a name for himself, winning racing titles at northern California racetracks including a victory in the 1981 California Derby. Baze went on to lead United States thoroughbred horse racing in victories ten times. He has won 36 riding titles at Bay Meadows racetrack in San Mateo, California and 27 titles at Golden Gate Fields in Albany, California.

After winning 400 or more races in a year for four consecutive years, Baze got his big break by being honored with a special Eclipse Award in 1995. Since then he has won 400 or more races in a year seven additional times; no other jockey has accomplished that feat more than three times.

In 1999, Baze was inducted into the National Museum of Racing and Hall of Fame and in 2002, he was voted the recipient of the prestigious George Woolf Memorial Jockey Award by his peers. Since the inauguration of the Isaac Murphy Award in 1995, presented annually by the National Turf Writers Association to the jockey with the highest winning percentage in North America, Baze has won it 13 of 14 years, coming in second in 2004.

Achievements
On October 14, 1989, Baze was aboard Hawkster when that three-year-old colt set the Santa Anita Park track record for 1$1/2$ miles on turf. Baze gained a lot more fame in the fourth race at Bay Meadows on December 1, 2006, by setting the world's all-time record for most career victories, passing jockey Laffit Pincay Jr., by winning career race 9,531 aboard Butterfly Belle, owned by Jim Pitzer Sr. of Washington. Among other noteworthy accomplishments, during the two days of October 17 and 18, 2007, Baze won eleven races.

Although he had won every other stakes race at Golden Gate Fields, Russell had never won the track's most prestigious race: the San Francisco Breeders' Cup Mile. That changed on April 24, 2010 when he took the race on Bold Chieftain from the pacesetter, Monterey Jazz.

Milestones
On February 1, 2008, at Golden Gate Fields, Baze rode Two Step Cat to a photo finish victory in the third race to become the first North American rider to win 10,000 races. On August 14, 2010, in the fourth race at the Sonoma County Fairgrounds in Santa Rosa, California, Baze rode Separate Forest, a first-time starter, to his 11,000th win.

On July 7, 2013, in Pleasanton, California, riding Handful of Pearls, Baze won the final race on the last day of the Alameda County Fair, making it his 12,000th win and his 4th win of the day.

Personal life
Baze and his wife Tami have four children. Their daughter Trinity is married to former jockey Kyle Kaenel, whose father, Jack Kaenel, won the Preakness Stakes at age 16.

title: Russell Baze


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User talk:Rrandolph

Karla Homolka
Hi: You are doing great work on this article. Do keep it up. When you write on talk pages you can sign and timestamp your post by entering four tildes ( ~ ) and they will be converted when you save the change. Furthermore, if you go to preferences and enter  Rrandolph ]] [[User_talk:Rrandolph|(Talk)  in the Your name (for signatures) box, you will have a signature with a talk page link in it like mine. You seem to know what were you doing; have you been an anonymous editor for a while before creating this account? --Theo (Talk) 15:08, 15 Jun 2005 (UTC)

Talk pages
Hi: You said that talk pages were non-intuitive. Please expand on that and I will see if I can help future newcomers find things simpler. You may find Introduction helpful as a first guide to this remarkable environment.—Theo (Talk) 16:20, 20 Jun 2005 (UTC)

license: Creative Commons - Attribution Share-Alike - https://creativecommons.org/licenses/by-sa/4.0/

title: User talk:Rrandolph


text:
Mamadou Diallo

Mamadou Diallo may refer to:

 * Mamadou Diallo (footballer, born 1971), Senegalese footballer
 * Mamadou Alimou Diallo (born 1984), Guinean football defender
 * Mamadou Diallo (athlete) (born 1954), Senegalese track and field athlete
 * Mamadou Diallo (footballer, born 1982), Malian footballer
 * Mamadou Diallo (judoka) (born 1941), Guinean Olympic judoka
 * Mamadou Diallo (wrestler), Mauritanian wrestler
 * Mamadou Diaw Diallo, Guinean wrestler
 * Mamadou Diallo (footballer, born 1990), Guinean football forward who played for Hougang United FC
 * Mamadou Diallo (footballer, born 1994), Guinean football forward who plays for Grenoble
 * Mamadou Diallo (footballer, born 1995), Guinean football forward who plays for Águia FC Vimioso
 * Mamadou Diallo (footballer, born 1997), Guinean football forward who plays for Energetik-BGU Minsk
 * Mamadou Sylla Diallo (born 1994), Senegalese footballer
 * Mamadou Mariem Diallo (born 1967), Senegalese footballer

title: Mamadou Diallo


text: File:Rhapsody dawn of victory.jpg

title: File:Rhapsody dawn of victory.jpg


text: Talk:Index of Baekje-related articles

title: Talk:Index of Baekje-related articles


text:
Talk:Seaside, Oregon

POV info moved from main page
"Every summer the population of Seaside increases double. And theyre there for one thing only- The Beach! When theyre at the beach they want to play in the water and the place they go is the Seaside Surf Shop located on the main highway coming into town. They have wetsuits, surfboards, and bodyboards for familys to rent and enjoy. For the less adventurous, you can go to the Prom Bike Shop and rent bicycles to cruise around town. The Fourth of July is the peak of the season and everything speeds up from there. The hiking up on the Tillamook head is insane and fun. Theres an Arcade downtown that you can take the kids to, it has bumper cars video games, taffy parlors, elephant ears, you name it."

The way this is currently written, it is unencyclopedic, sounds like original research, uses the wrong person (second person), and sounds like an advertisement for the surf shop and bike shop. Please read about what Wikipedia is not so you can understand what we are looking for. In a nutshell: Wikipedia is not a tourist guide, and we strive to maintain a neutral point of view, which means leaving out words like "insane" and "fun". Thanks. Katr67 19:14, 21 December 2006 (UTC)

West Seaside
A City of West Seaside was incorporated in 1905. Aboutmovies (talk) 08:47, 22 December 2009 (UTC)

 * See also this discussion about 1891 city Ocean Grove. Katr67 (talk) 17:51, 22 December 2009 (UTC)

Rick Still
I added that Rick Still from from here because he was a local D.J. for a while.--Thunderpilot (talk) 22:36, 15 February 2013 (UTC)
 * Do you have a reference that can be cited? Currently, there's no ref here nor in his article that supports a connection to the city. --- Barek (talk • contribs) - 00:02, 16 February 2013 (UTC)

(I put in that he was a DJ at a radio station in Seaside Oregon. http://www.youtube.com/watch?v=rmpKlnesGpI and Madness ensues as Consumption and KSWB DJ Rick Still adlib 2 radio ads. Presented by Viral Media Inc. is the Youtube video--Thunderpilot (talk) 01:10, 16 February 2013 (UTC) Also on youtube go to rick still radio. That is one of his channels there.--Thunderpilot (talk) 01:17, 16 February 2013 (UTC) http://www.youtube.com/user/RickStillRadio Rick Still has videos about being in Seaside Oregon while working at the radio station.--Thunderpilot (talk) 01:27, 16 February 2013 (UTC)

Title
Why the name is "Seaside, Oregon" instead of "Seaside (Oregon)"? --Andyrom75 (talk) 17:02, 20 March 2013 (UTC)
 * This article is about a city in Oregon named Seaside; according to the article naming disambiguation guidelines this is the proper way to write it. If the article were about generic seashore in Oregon, that would be written Seashore (Oregon) per the same guidelines.  —EncMstr (talk) 18:10, 20 March 2013 (UTC)

schools and tsunami inundation zones? ?
Seaside Voters Back Bond To Move Schools From Tsunami Zone, OPB [Oregon Public Broadcasting], by R.J. Marx, Daily Astorian | Nov. 9, 2016.

'Seaside School District voters said a resounding “yes” Tuesday to a $99.7 million bond to move three schools out of the tsunami inundation zone.

'In a 65 percent to 35 percent vote, residents endorsed the plan to replace deteriorating schools at an 80-acre location in the city’s East Hills adjacent to Seaside Heights Elementary School. . .  '

' .  .  .  The bond came three years after a failed $128.8 million dollar plan. The scaled-back proposal eliminated an auditorium, covered bleachers, long-term emergency shelters and a varsity playing field. . .  .  A home with an assessed value of $200,000 would see a tax hike of about $270 and a $400,000 home about $540.'

 * Important subject. Now the article includes a photo which seems to be of another school district entirely of an elementary student hiding under his desk during a tsunami drill.  FriendlyRiverOtter (talk) 18:04, 4 February 2017 (UTC)

See also:

http://www.seaside.k12.or.us/

http://www.dailyastorian.com/Free/20161108/voters-backing-seaside-schools-bond

The Really Small Ones, New Yorker, Kathryn Schulz, Nov. 4, 2016.

other potentially good article(s) on tsunami defense
http://www.academia.edu/6168915/A_Tsunami_Defense_Mechanism

 * want to take good long look and might reference us to some other articles. FriendlyRiverOtter (talk) 21:10, 2 March 2017 (UTC)

http://www.times-standard.com/article/NJ/20170322/LOCAL1/170329950 EDITORIAL Lori Dengler is an emeritus professor of geology at Humboldt State University, an expert in tsunami and earthquake hazards and co-author of “The Extraordinary Voyage of Kamome,” from which proceeds support the Japanese-Crescent City student exchanges and outreach efforts.

 * shows that it is a real issue. FriendlyRiverOtter (talk) 20:29, 24 March 2017 (UTC)

External links modified
Hello fellow Wikipedians,

I have just modified 4 external links on Seaside, Oregon. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:
 * Added archive http://www.webcitation.org/6HQu4Spqa?url=http://www.census.gov/popest/data/cities/totals/2012/SUB-EST2012.html to http://www.census.gov/popest/data/cities/totals/2012/SUB-EST2012.html
 * Added archive http://www.webcitation.org/699nOulzi?url=http://www.census.gov/geo/www/gazetteer/files/Gaz_places_national.txt to http://www.census.gov/geo/www/gazetteer/files/Gaz_places_national.txt
 * Added archive https://archive.is/20160602200744/http://www.census.gov/popest/data/cities/totals/2015/SUB-EST2015.html to http://www.census.gov/popest/data/cities/totals/2015/SUB-EST2015.html
 * Added archive http://arquivo.pt/wayback/20090709154837/http%3A//www%2Ecensus%2Egov/popest/cities/files/SUB%2DEST2007%2D41%2Ecsv to http://www.census.gov/popest/cities/files/SUB-EST2007-41.csv

When you have finished reviewing my changes, you may follow the instructions on the template below to fix any issues with the URLs.

Cheers.— InternetArchiveBot  (Report bug) 22:09, 21 May 2017 (UTC)

Snowy Winters?
The climate section says "Seaside has a typical Pacific Northwest coastal climate, receiving snowy winters and mild-to-cool summers." This seems like an error and they meant to say rainy. Snowy winters are not typical of the Northwest coast, and for Seaside in particular the sources I found say it has an annual average snowfall of zero.

https://www.currentresults.com/Weather/Oregon/annual-snowfall.php Dansan99 (talk) 08:40, 12 September 2018 (UTC)

title: Talk:Seaside, Oregon


text:
Talk:Mashup

Redirect
i'm curious as to how the term "mashup" gained any credibility as a word. mashup? really? that's something you do with potatoes. anyway, you're free to delete this sentence. —Preceding unsigned comment added by 98.88.77.174 (talk) 01:13, 6 February 2011 (UTC)

chocolateboy - I'm curious as to why you recently removed the generalized mashup entry and reinstated the redirect to a specialized entry with a limited scope. If you intend to revert again, could you please post justifications here?

 * Sure. It's unexpected, unencyclopaedic and unsubstantiated. This isn't UrbanDictionary.

 * chocolateboy 21:51, 15 Jun 2005 (UTC)

Bastard Pop
I haven't seen the entry Chocolateboy removed, but I'd like to share a couple of thoughts: 1) NOBODY but NOBODY who DOES it calls it "Bastard pop". Anywhere. Nor have I EVER seen that term outside of *here*. 2) This is a new and evolving terminology; when there is no body of research with any substance, "original research" in the sense of "I've heard of the term many times, and am familiar with the subculture that spawned it" is the only recourse. Of course adding citations (in this case, "how to make a mashup" for example) would substantiate not only the article but also the proper term, which in this case IS "Mashup"; 3) This may be a perfect example of the kind of "edit" which is driving people away from Wikipedia; 4) "Bastard pop" is a pejorative term for something many of us are fond of. So, Chocolate *boy*, consider easing up. THere are some other principles for Wikipeda, which include RESPECT. Just a little hint. Twang 00:35, 6 March 2006 (UTC)

 * I haven't seen the entry Chocolateboy removed

 * Just to clarify what you're "defending" in place of the current disambiguation page, here it is:

 * see Bastard pop for a thorough investigation of musical mashups.

 * "mashup" on a larger scale refers to a general aesthetic /ethic of 'reduce, reuse, recycle' + 'steal & pillage' practically applied to an artform/trade/technology (or combination thereof)...

 * very DIY.

 * NOBODY but NOBODY who DOES it calls it "Bastard pop".

 * Reliable sources     and bootleggers       &c. disagree.

 * "Mashup" or "mashups" are no more a substitute for "bastard pop" as the title of the article than "raps" or "breaks" are for hip hop or drum and bass. These articles are about the genre, not the names given to its songs or techniques. These names are mentioned prominently in the article and are linked or redirected as appropriate. At any rate, this dab isn't going anywhere. Mashup (web application hybrid) is the first link Google finds when searching for "mash-up" and the second for "mashup". "Mashup" (of course) traditionally referred to reggae mixes, so even if there was no competition from webapps, it would still suffer from the same ambiguity as "cut-up" and "bootleg".

 * As for your other points, see Reliable sources, Verifiability, Cite sources, No original research, and Check your facts.

 * chocolateboy 01:18, 7 March 2006 (UTC)

 * In this particular case, Google is not a good authority to appeal to, as Google Inc promotes mindshare by encouraging programmers to create "mashups" using their technology. Yahoo search has the first two links pointing to Wikipedia, followed by two music sites. As far as sources go, links to Wikipedia shouldn't be used as verification for Wikipedia.
 * And re: this "dab" not going anywhere, only time will tell how long a "web application hybrid" remains notable enough for the 'pedia. Shoehorn 02:53, 1 July 2006 (UTC)

 * You're not wrong.

 * And I'm more than happy to aquiesce to the status quo when there is a status quo. It's a bit of a shame (IMHO) that "mashup" is a dab rather than a link that explains how the web epigone earned its name...

 * But "Bastard Pop" is the formal name for the genre, and "mashups" is the ubiquitous (and at least one-third ambiguous) name for bastard pop songs. "Bastard Pop" is less encumbered by ambiguity and clearer than "Mashup (music)". 1/3 is not feeble enough to kick a competing namespace to the kerb. Would you really prefer Wikipedia articles to be called "Mashup (music)" rather than "Bastard Pop", "Jungle" (or "breaks" or "breakbeats") rather than "Drum & Bass" or "Rap" rather than "Hip Hop"?

 * chocolateboy 00:03, 6 July 2006 (UTC)

 * There are distinctions to be made between jungle and drum and bass, and rap and hip hop, and I'd rather go for clarity through context than trying to force a "better" classification where it isn't wanted. Even calling it a genre is a big strong, discogs.com categorizes the genre of most of the examples from the bastard pop article as either electronic, hip hop, or both. I also don't find "mashup" to be a popular metonym for "song" or "track". A mashup is ultimately just a technique for mixing music, akin to the use of multi-track magnetic tape. Shoehorn 06:18, 6 July 2006 (UTC)

 * Even calling it a genre is a big strong

 * No it isn't.

 * discogs.com is irrelevant. It doesn't have a bastard pop or mashup tag. It also doesn't have a crunk, reggaeton, grime (music), punk, j-pop or techno tag. Do you really think that somehow proves that those genres/subgenres don't exist or that the terms are incorrect?

 * A mashup is ultimately just a technique for mixing music

 * Feel free to add an article about the "technique" (I don't see how it differs in any way from hip hop or any other form of sampling as far as the technique goes), akin to the scratching or toasting articles. The bastard pop article, however, is about the genre.

 * chocolateboy 10:26, 6 July 2006 (UTC)

 * I find discogs to be surprisingly conservative in their classification. I think WP would benefit from a similar attitute wrt music and music culture, I don't think trying to trace the ongoing development of genres/subgenres is something we should be doing (crystal ball and all that). And I don't see why you are so dead set on this "bastard pop" classification, cite me something out of an actual music print publication (Rolling Stone?) instead of the disposable Salon.com. Shoehorn 10:45, 6 July 2006 (UTC)

 * I think WP would benefit from a similar attitute wrt music and music culture

 * Then I suggest you resume your campaign here when you've persuaded the editors of the abovementioned articles to delete or rename them. Good luck with that.

 * cite me something out of an actual music print publication (Rolling Stone?)

 * You're gonna have to point out the policy page that says a music article must justify its title or existence with a reference to a Rolling Stone article. I've searched high and low and can't find it anywhere. They (Rolling Stone) also, apparently, haven't heard of:

 * Mathcore
 * 65daysofstatic
 * Aberfeldy
 * Julie Covington
 * Meck
 * Mystery Jets
 * Nathan Fake
 * Nolwenn Leroy
 * Product.01
 * Shapeshifters
 * The Elgins
 * The Happy Bullets

 * &c.

 * Sounds like a bug in Rolling Stone to me. If you have a problem with the credibility of the Sydney Morning Herald, mp3.com, Paul Morley, Salon, The New Yorker, Wired and The Guardian, then I suggest you take it up on the talk pages of Reliable sources, Verifiability, Cite sources and No original research.

 * chocolateboy 18:56, 7 July 2006 (UTC)

 * Did you forget to make a point there somewhere?
 * mashup music  12,900,000 hits on google
 * "bastard pop" music 159,000 hits on google
 * You can continue to cherry pick articles from Salon, The New Yorker, ad nauseum, but it won't change the fact that "bastard pop" was never the popular term. Shoehorn 23:09, 7 July 2006 (UTC)

 * I've made 33 referenced points. You've just contradicted yourself again. Google is biased. Google is reliable. "Music print" sources are the only reliable sources. Google is a reliable source. Wikipedia should be surprisingly conservative. Wikipedia should keep its finger on the pulse of the Google zeitgeist. It's not a genre. The genre is called "mashup" [sic]. Wikipedia should limit itself to the handful of categories used by discogs.com. Wikipedia should "innovate" and "invent" a new "mashup" category, just for this "crystal ball"-gazing article, which shouldn't really exist anyway.

 * The stats for "bastard pop" vs "mashup" are as irrelevant as the stats for "rap" vs "hip hop" and "breaks"/"jungle" vs "drum and bass" for reasons outlined ad nauseam above and here.

 * chocolateboy 05:05, 8 July 2006 (UTC)

The bastard pop article is a piece of shit anyway. You can have it, chocolateboy. Shoehorn 08:36, 8 July 2006 (UTC)

Once upon a time someone called it Bastard pop
But it is and always will be Mashups or Mash-Ups. Problem is that Hybrid Web 2.0 APIs are now using the term Mashups. But that's a recent thing.

Bastard Pop is a correct way to describe Music Hybrids, but Mashups is more relevant.

What to do eh?

I vote for the Mashups Disambiguation page to refer to "Mashup (web application hybrid)" and "Mashup (Music Hybrid)".

Bastard pop will disappear faster than it was coined as a term. Listen to any radio station or serach the web - Mashups is always used and you NEVER hear the term Bastard Pop.

My 2c —Preceding unsigned comment added by 166.214.6.229 (talk • contribs)

 * My 50 Cent :-) is that this is an encyclopedia, not a blog.

 * chocolateboy 05:57, 2 August 2006 (UTC)

Jamaican derivation
I'm interested to see the entry discuss the Jamaican patois derivation of the word. Do dictionary definitions belong here? If so, I'll have a go at writing a better one, but I wanted to check in first.

If at all, I think the idea is to disambiguate the term in different musical contexts - "mash up"/"mashin up" in the reggae/ska context and "mashup" in the "combining sources" sense - in Jamaica at least, there is also the sense of destruction ie 'the police dem mash up me head'

How?
How is this lame ass article on wikipedia? I looked at the Wikipedia logo to the left just to check it wasnt Encyclopedia Dramatica.

Mashme Project
Hello there. I do not have too much experience with Wikipedia. I did my B.A. project on Mashups and I'd like to share it with whoever thinks it might be useful to him. On the website there is a multimedia approach to explain this topic. There are simple explanation in textform, embedded video examples and audio interviews from people like Lawrence Lessig. Furthermore there are selected links to scientific rescources.

The url is www.mashme.info. Feel free to use, recycle and link to it. It is under the creative commons Attribution/Share-Alike License.

cheers —Preceding unsigned comment added by 78.48.139.68 (talk) 11:35, 27 July 2009 (UTC)

Mashup minded
Can we put a direction to mashup minded here? -Michael.kutch (talk) 21:46, 26 October 2009 (UTC)

Music vs. Culture
Tag lines for "mash-up (culture)" and "mash-up (music)" are confusingly similar on the current disambig page. Somebody fix this please? Morganfitzp (talk) 19:47, 11 February 2019 (UTC)

title: Talk:Mashup


text:
Wikipedia talk:WikiProject Doctor Who/sandbox

What should the title for series be for Doctor Who and the Pescatons? Something like released separately? --bjwebb 15:10, 15 Jun 2005 (UTC)

 * No need for a series header - just audio plays will do, IMO. --khaosworks 15:23, Jun 15, 2005 (UTC)


text:
Piper oilfield

The Piper oilfield is a substantial North Sea oilfield covering 30.1 km2 (11½ sq. mi.). It lies roughly halfway between Aberdeen and Bergen, at the eastern end of the Moray Firth basin. Oil extracted from it is piped to Scotland, where it is stabilised at an oil plant on the island of Flotta, in the Orkney archipelago, while gas is shipped via the Frigg gas pipeline. In June 1975, the Piper Alpha oil platform was placed over the field in 144 metres (79 fathoms) of water, secured in place by 24 piles extending 116 metres (63 fathoms) beneath the seabed. The platform was designed for simultaneous drilling and production. Piper Alpha was the site of one of the world's worst oil platform disasters when it was destroyed by an explosion in 1988, with the loss of 167 lives. Piper Bravo was installed in 1992. Talisman Energy acquired a controlling interest in 2000.

Occidental Petroleum Corp., Getty Oil (Britain) Ltd., Thomson North Sea Ltd., and Allied Chemical (North Sea) Ltd., that later transformed into the OPCAL joint venture, obtained an oil exploration licence in 1972 and discovered the Piper oilfield in early 1973 after seismically mapping the area. Oil production started in 1976 with about 250000 oilbbl/d increasing to 300000 oilbbl/d. A gas recovery module was installed by 1980. Production declined to 125000 oilbbl/d by 1988. OPCAL built the Flotta oil terminal in the Orkney Islands to receive and process oil from the Piper, Claymore and Tartan fields, each with its own platform. A 30 in diameter main oil pipeline ran 128 mi from Piper Alpha to Flotta, with a short oil pipeline from the Claymore platform joining it some 20 mi to the west. The Tartan field also fed oil to Claymore and then onto the main line to Flotta. Separate 46 cm (18") diameter gas pipelines run from Piper to the Tartan platform, and from Piper to the gas compressing platform MCP-01 some 30 mi to the northwest.

Geology
The field consists of three folded, tilted blocks on the northern edge of the Witch Ground Graben. Production is from the Upper Jurassic Piper Sandstone, a sandstone shelf with a thickness up to 142 metres (465') and Oil-water contact ranging in depths from 2195 to 2804 metres (7201' to 9200') under the sea. Piper oil most likely originated in the Kimmeridge Shale.

title: Piper oilfield


text:
Skufia

A skufia (also skufiya, skoufia or skoufos; σκούφια or σκούφος) is an item of clerical clothing, a cap, worn by Eastern Orthodox, Eastern Lutheran and Eastern Catholic monastics (in which case it is black) or awarded to clergy as a mark of honor (in which case it is usually red or purple).

Description
A skufia is a soft-sided brimless cap whose top may be pointed (Russian style), flat and pleated (Greek style), or flat with raised edges (Romanian style). Typically, monastics receive their skufia either when they first become a novice or when they are tonsured. A monk or nun who has been tonsured to the Great Schema will wear a skoufia that has been embroidered with prayers, crosses, and figures of seraphim.

High-ranking bishops (such as archbishops and metropolitans) will sometimes wear a black or purple skufia with a small jewelled cross on informal occasions. A nun will sometimes wear a skufia over her monastic veil; while monks often wear the skufia (without a veil) when the klobuk or epanokamelavkion might get in the way of work.

title: Skufia


text:
Mosasaurus

Mosasaurus ("lizard of the Meuse River") is the type genus (defining example) of the mosasaurs, an extinct group of aquatic squamate reptiles. It lived from about 82 to 66 million years ago during the Campanian and Maastrichtian stages of the Late Cretaceous. The genus was one of the first Mesozoic marine reptiles known to science—the first fossils of Mosasaurus were found as skulls in a chalk quarry near the Dutch city of Maastricht in the late 18th century, and were initially thought to be crocodiles or whales. One skull discovered around 1780 was famously nicknamed the "great animal of Maastricht". In 1808, naturalist Georges Cuvier concluded that it belonged to a giant marine lizard with similarities to monitor lizards but otherwise unlike any known living animal. This concept was revolutionary at the time and helped support the then-developing ideas of extinction. Cuvier did not designate a scientific name for the animal; this was done by William Daniel Conybeare in 1822 when he named it Mosasaurus in reference to its origin in fossil deposits near the Meuse River. The exact affinities of Mosasaurus as a squamate remain controversial, and scientists continue to debate whether its closest living relatives are monitor lizards or snakes.

Traditional interpretations have estimated the maximum length of the largest species, M. hoffmannii, to be 17.1 m, making it one of the largest mosasaurs, although some scientists consider this an overestimation with recent estimates suggesting a length closer to 13 m. The skull of Mosasaurus had robust jaws and strong muscles capable of powerful bites using dozens of large teeth adapted for cutting prey. Its four limbs were shaped into paddles to steer the animal underwater. Its tail was long and ended in a downward bend and a paddle-like fluke. Mosasaurus possessed excellent vision to compensate for its poor sense of smell, and a high metabolic rate suggesting it was endothermic ("warm-blooded"), an adaptation in squamates only found in mosasaurs. There is considerable morphological variability across the currently-recognized species in Mosasaurus—from the robustly-built M. hoffmannii to the slender and serpentine M. lemonnieri—but an unclear diagnosis (description of distinguishing features) of the type species M. hoffmannii led to a historically problematic classification. As a result, more than fifty species have been attributed to the genus in the past. A redescription of the type specimen in 2017 helped resolve the taxonomy issue and confirmed at least five species to be within the genus. Another five species still nominally classified within Mosasaurus are planned to be reassessed.

Fossil evidence suggests Mosasaurus inhabited much of the Atlantic Ocean and the adjacent seaways. Mosasaurus fossils have been found in North and South America, Europe, Africa, Western Asia, and Antarctica. This distribution encompassed a wide range of oceanic climates including tropical, subtropical, temperate, and subpolar. Mosasaurus was a common large predator in these oceans and was positioned at the top of the food chain. Paleontologists believe its diet would have included virtually any animal; it likely preyed on bony fish, sharks, cephalopods, birds, and other marine reptiles including sea turtles and other mosasaurs. It likely preferred to hunt in open water near the surface. From an ecological standpoint, Mosasaurus probably had a profound impact on the structuring of marine ecosystems; its arrival in some locations such as the Western Interior Seaway in North America coincides with a complete turnover of faunal assemblages and diversity. Mosasaurus faced competition with other large predatory mosasaurs such as Prognathodon and Tylosaurus—which were known to feed on similar prey—though they were able to coexist in the same ecosystems through niche partitioning. There were still conflicts among them, as an instance of Tylosaurus attacking a Mosasaurus has been documented. Several fossils document deliberate attacks on Mosasaurus individuals by members of the same species. In fighting likely took place in the form of snout grappling, as seen in modern crocodiles.

Discovery and identification
The first Mosasaurus fossil known to science was discovered in 1764 in a chalk quarry near Maastricht in the Netherlands in the form of a skull, which was initially identified as a whale. This specimen, cataloged as TM 7424, is now on display at the Teylers Museum in Haarlem. Later around 1780, the quarry produced a second skull that caught the attention of the physician Johann Leonard Hoffmann, who thought it was a crocodile. He contacted the prominent biologist Petrus Camper, and the skull gained international attention after Camper published a study identifying it as a whale. This caught the attention of French revolutionaries, who looted the fossil following the capture of Maastricht during the French Revolutionary Wars in 1794. In a 1798 narrative of this event by Barthélemy Faujas de Saint-Fond, the skull was allegedly retrieved by twelve grenadiers in exchange for an offer of 600 bottles of wine. This story helped elevate the fossil into cultural fame, but historians agree that the narrative was exaggerated.

After its seizure, the second skull was sent to the National Museum of Natural History, France in 1795 and later cataloged as MNHN AC 9648. By 1808, Camper's son Adriaan Gilles Camper and Georges Cuvier concluded that the fossil, which by then was nicknamed the "great animal of Maastricht", belonged to a marine lizard with affinities to monitor lizards, but otherwise unlike any modern animal. The skull became part of Cuvier's first speculations about the conception of extinction, which later led to his theory of catastrophism, a precursor to the theory of evolution. At the time, it was not believed that a species could go extinct, and fossils of animals were often interpreted as some form of an extant species. Cuvier's idea that there existed an animal unlike any today was revolutionary at the time, and in 1812 he proclaimed, "Above all, the precise determination of the famous animal from Maastricht seems to us as important for the theory of zoological laws, as for the history of the globe." In a 1822 work by James Parkinson, William Daniel Conybeare coined the genus Mosasaurus from the Latin Mosa "Meuse" and the Ancient Greek σαῦρος (saûros, "lizard"), all literally meaning "lizard of the Meuse", in reference to the river where the holotype specimen was discovered nearby. In 1829, Gideon Mantell added the specific epithet hoffmannii, in honor to Hoffmann. Cuvier later designated the second skull as the new species' holotype (defining example).

Other species
In 1804, the Lewis and Clark Expedition discovered a now-lost fossil skeleton alongside the Missouri River, which was identified as a 45 ft long fish. Richard Ellis speculated in 2003 that this may have been the earliest discovery of the second species M. missouriensis, although competing speculations exist. In 1818, a fossil from Monmouth County, New Jersey became the first North American specimen to be correctly recognized as a Mosasaurus by scientists of the time.

The type specimen of M. missouriensis was first described in 1834 by Richard Harlan based on a snout fragment found along the river's Big Bend. He coined the specific epithet and initially identified it as a species of Ichthyosaurus but later as an amphibian. The rest of the skull had been discovered earlier by a fur-trapper, and it eventually came under the possession of prince Maximilian of Weid-Neuwied between 1832 and 1834. The fossil was delivered to Georg August Goldfuss in Bonn for research, who published a study in 1845. The same year, Christian Erich Hermann von Meyer suspected that the skull and Harlan's snout were part of the same individual. This was confirmed in 2004.

The third species was described in 1881 from fragmentary fossils in New Jersey by Edward Drinker Cope, who thought it was a giant species of Clidastes and named it Clidastes conodon. In 1966, it was reidentified as a species of Mosasaurus. In his description, Cope does not provide the etymology for the specific epithet conodon, but it is suggested that it could be a portmanteau meaning "conical tooth", derived from the Ancient Greek κῶνος (kônos, "cone") and ὀδών (odṓn, "tooth"), probably in reference to conical surface teeth smooth of the species.

The fourth species M. lemonnieri was first detected by Camper Jr. based on fossils from his father's collections, which he discussed with Cuvier during their 1799 correspondence, but Cuvier rejected the idea of another Mosasaurus species. This species was re-introduced to science and formally described in 1889 by Louis Dollo based on a skull recovered by Alfred Lemonnier from a phosphate quarry in Belgium. Dollo names the species in his honor. Further mining of the quarry in subsequent years uncovered many additional well-preserved fossils, including multiple partial skeletons which collectively represented nearly the entire skeleton of the species. They were described by Dollo in later papers. Despite being the best anatomically represented species, M. lemonnieri was largely ignored in scientific literature. Theagarten Lingham-Soliar suggested two reasons for this neglect. First, M. lemonnieri fossils are endemic to Belgium and the Netherlands, which despite the famous discovery of the M. hoffmannii holotype attracted little attention from mosasaur paleontologists. Second, the species was overshadowed by the more famous and history-rich type species.

M. lemonnieri is a controversial taxon, and there is debate on whether it is a distinct species or not. In 1967, Dale Russell argued that M. lemonnieri and M. conodon are the same species and designated the former as a junior synonym per the principle of priority. In a 2000 study, Lingham-Soliar refuted this based on a comprehensive study of existing M. lemonnieri specimens, which was corroborated by a study on the M. conodon skull by Takehito Ikejiri and Spencer G. Lucas in 2014. In 2004, Eric Mulder, Dirk Cornelissen, and Louis Verding suggested M. lemonnieri could be a juvenile form of M. hoffmannii based on the argument that significant differences could be explained by age-based variation. However, the need for more research to confirm any hypotheses of synonymy was expressed.

The fifth species M. beaugei was described by Camille Arambourg in 1952 from isolated teeth originating from phosphate deposits in the Oulad Abdoun Basin and the Ganntour Basin in Morocco. The species is named in honor of Alfred Beaugé, director at the time of the OCP Group, who invited Arambourg to participate in the research project and helped him to provide local fossils.

Early depictions
Scientists during the early and mid-1800s initially imagined Mosasaurus as an amphibious marine reptile with webbed feet and limbs for walking. This was based on fossils like the M. missouriensis holotype, which indicated an elastic vertebral column that Goldfuss in 1845 saw as evidence of an ability to walk and interpretations of some phalanges as claws. In 1854, Hermann Schlegel proved how Mosasaurus actually had fully aquatic flippers. He clarified that earlier interpretations of claws were erroneous and demonstrated how the phalanges show no indication of muscle or tendon attachment, which would make walking impossible. They are also broad, flat, and form a paddle. Schlegel's hypothesis was largely ignored by contemporary scientists but became widely accepted by the 1870s when Othniel Charles Marsh and Cope uncovered more complete mosasaur remains in North America.

One of the earliest depictions of Mosasaurus in paleoart is a life-size concrete sculpture created by Benjamin Waterhouse Hawkins between 1852 and 1854 as part of the collection of sculptures of prehistoric animals on display at the Crystal Palace Park in London. The restoration was primarily informed by Richard Owen's interpretation of the M. hoffmannii holotype and the anatomy of monitor lizards, so Hawkins depicted the animal as essentially a water-going monitor lizard. It was given a boxy head, nostrils at the side of the skull, large volumes of soft tissue around the eyes, lips reminiscent of monitor lizards, scales consistent with those in large monitors like the Komodo dragon, and a flipper. The model was deliberately sculpted incomplete, which Mark Witton believed was likely to save time and money. Many elements of the sculpture can be considered inaccurate, even for the time. It did not take into account Golduss' 1845 study of M. missouriensis which instead called for a narrower skull, nostrils at the top of the skull, and amphibious terrestrial limbs (the latter being incorrect in modern standards ).

Description
Mosasaurus was a type of derived mosasaur, or a latecoming member with advanced evolutionary traits such as a fully aquatic lifestyle. As such, it had a streamlined body, an elongated tail ending with a downturn supporting a two-lobed fin, and two pairs of flippers. While in the past derived mosasaurs were depicted as akin to giant flippered sea snakes, it is now understood that they were more similar in build to other large marine vertebrates such as ichthyosaurs, marine crocodylomorphs, and archaeocete whales through convergent evolution.

Size
The type species, M. hoffmannii, is one of the largest marine reptiles known, though knowledge of its skeleton remains incomplete as it is mainly known from skulls. Russell (1967) wrote that the length of the jaw equalled one tenth of the body length in the species. Based on this ratio, Grigoriev (2014) used the largest lower jaw attributed to M. hoffmannii (CCMGE 10/2469, also known as the Penza specimen; measuring 171 cm in length) to estimate a maximum length of 17.1 m. Using a smaller partial jaw (NHMM 009002) measuring 90 cm and "reliably estimated at" 160 cm when complete, Lingham-Soliar (1995) estimated a larger maximum length of 17.6 m via the same ratio. No explicit justification for the 1:10 ratio was provided in Russell (1967), and it has been considered to be probably overestimated by Cleary et al. (2018). In 2014, Federico Fanti and colleagues alternatively argued that the total length of M. hoffmannii was more likely closer to seven times the length of the skull, which was based on a near-complete skeleton of the related species Prognathodon overtoni. The study estimated that an M. hoffmannii individual with a skull measuring more than 145 cm would have been up to or more than 11 m in length and weighed 10 MT in body mass.

Isolated bones suggest some M. hoffmannii may have exceeded the lengths of the Penza specimen. One such bone is a quadrate (NHMM 003892) which is 150% larger than the average size, which Everhart and colleagues in 2016 reported can be extrapolated to scale an individual around 18 m in length. It was not stated whether they applied Russell's 1967 ratio.

M. missouriensis and M. lemonnieri are smaller than M. hoffmannii but are known from more complete fossils. Based on measurements of various Belgian skeletons, Dollo estimated M. lemonnieri grew to around 7 to 10 m in length. He also measured the dimensions of IRSNB 3119 and recorded that the skull constituted approximately one-eleventh of the whole body. Polcyn et al. (2014) estimated that M. missouriensis may have measured up to 8-9 m in length. Street (2016) noted that large M. missouriensis individuals typically had skulls exceeding lengths of 1 m. A particular near-complete skeleton of M. missouriensis is reportedly measured at 6.5 m in total length with a skull approaching 1 m in length. Based on personal observations of various unpublished fossils from Morocco, Nathalie Bardet et al. (2015) estimated that M. beaugei grew to a total length of 8-10 m, their skulls typically measuring around 1 m in length. With a skull measuring around 97.7 cm in length, M. conodon has been regarded as a small to medium-sized representative of the genus.

Skull
The skull of Mosasaurus is conical and tapers off to a short snout which extends a little beyond the frontmost teeth. In M. hoffmannii, this snout is blunt, while in M. lemonnieri it is pointed. Above the gum line in both jaws, a single row of small pits known as foramina are lined parallel to the jawline; they are used to hold the terminal branches of jaw nerves. The foramina along the snout form a pattern similar to the foramina in Clidastes skulls. The upper jaws in most species are robustly built, broad, and deep except in M. conodon, where they are slender. The disparity is also reflected in the dentary, the lower jawbone, although all species share a long and straight dentary. In M. hoffmannii, the top margin of the dentary is slightly curved upwards; this is also the case with the largest specimens of M. lemonnieri, although more typical skulls of the species have a near-perfectly straight jawline. The premaxillary bar, the long portion of the premaxillary bone extending behind the premaxillary teeth, is narrow and constricts near the middle in M. hoffmannii and M. lemonnieri like in typical mosasaurs. In M. missouriensis, the bar is robust and does not constrict. The external nares (nostril openings) are moderately sized and measure around 21–24% of the skull's length in M. hoffmannii. They are placed further toward the back of the skull than in nearly all other mosasaurs (exceeded only by Goronyosaurus), and begin above the fourth or fifth maxillary teeth. As a result, the rear portions of the maxilla (the main tooth-bearing bone of the upper jaw) lack the dorsal concavity that would fit the nostrils in typical mosasaurs.

The palate, which consists of the pterygoid bones, palatine bone, and nearby processes of other bones, is tightly packed to provide greater cranial stability. The neurocranium housed a brain which was narrow and relatively small compared to other mosasaurs. For example, the braincase of the mosasaur Plioplatecarpus marshi provided for a brain around twice the size of that in M. hoffmannii despite being only half the length of the latter. Spaces within the braincase for the occipital lobe and cerebral hemisphere are narrow and shallow, suggesting such brain parts were relatively small. The parietal foramen in Mosasaurus, which is associated with the parietal eye, is the smallest among mosasaurids. The quadrate bone, which connected the lower jaw to the rest of the skull and formed the jaw joint, is tall and somewhat rectangular in shape, differing from the rounder quadrates found in typical mosasaurs. The quadrate also housed the hearing structures, with the eardrum residing within a round and concave depression in the outer surface called the tympanic ala. The trachea likely stretched from the esophagus to below the back end of the lower jaw's coronoid process, where it split into smaller pairs of bronchi which extended parallel to each other.

Teeth
The features of teeth in Mosasaurus vary across species, but unifying characteristics include a design specialized for cutting prey, highly prismatic surfaces (enamel circumference shaped by flat sides called prisms), and two opposite cutting edges. Mosasaurus teeth are large and robust except for those in M. conodon and M. lemonnieri, which instead have more slender teeth. The cutting edges of Mosasaurus differ by species. The cutting edges in M. hoffmannii and M. missouriensis are finely serrated, while in M. conodon and M. lemonnieri serrations do not exist. The cutting edges of M. beaugei are neither serrated nor smooth, but instead possess minute wrinkles known as crenulations. The number of prisms in Mosasaurus teeth can slightly vary between tooth types and general patterns differ between species—M. hoffmannii had two to three prisms on the labial side (the side facing outwards) and no prisms on the lingual side (the side facing the tongue), M. missouriensis had four to six labial prisms and eight lingual prisms, M. lemonnieri had eight to ten labial prisms, and M. beaugei had three to five labial prisms and eight to nine lingual prisms.

Like all mosasaurs, Mosasaurus had four types of teeth, classified based on the jaw bones they were located on. On the upper jaw, there were three types: the premaxillary teeth, maxillary teeth, and pterygoid teeth. On the lower jaw, only one type, the dentary teeth, were present. In each jaw row, from front to back, Mosasaurus had: two premaxillary teeth, twelve to sixteen maxillary teeth, and eight to sixteen pterygoid teeth on the upper jaw and fourteen to seventeen dentary teeth on the lower jaw. The teeth were largely consistent in size and shape with only minor differences throughout the jaws (homodont) except for the smaller pterygoid teeth. The number of teeth in the maxillae, pterygoids, and dentaries vary between species and sometimes even individuals—M. hoffmannii had fourteen to sixteen maxillary teeth, fourteen to fifteen dentary teeth, and eight pterygoid teeth;  M. missouriensis had fourteen to fifteen maxillary teeth, fourteen to fifteen dentary teeth, and eight to nine pterygoid teeth;  M. conodon had fourteen to fifteen maxillary teeth, sixteen to seventeen dentary teeth, and eight pterygoid teeth;  M. lemonnieri had fifteen maxillary teeth, fourteen to seventeen dentary teeth, and eleven to twelve pterygoid teeth;   and M. beaugei had twelve to thirteen maxillary teeth, fourteen to sixteen dentary teeth, and six or more pterygoid teeth. One indeterminate specimen of Mosasaurus similar to M. conodon from the Pembina Gorge State Recreation Area in North Dakota was found to have an unusual count of sixteen pterygoid teeth, far greater than in known species.

The dentition was thecodont (tooth roots deeply cemented within the jaw bone). Teeth were constantly shed through a process where the replacement tooth developed within the root of the original tooth and then pushed it out of the jaw. Chemical studies conducted on a M. hoffmannii maxillary tooth measured an average rate of deposition of odontoblasts, the cells responsible for the formation of dentin, at 10.9 um per day. This was by observing the von Ebner lines, incremental marks in dentin that form daily. It was approximated that it took the odontoblasts 511 days and dentin 233 days to develop to the extent observed in the tooth.

Postcranial skeleton
One of the most complete Mosasaurus skeletons in terms of vertebral representation (Mosasaurus sp.; SDSM 452) has seven cervical (neck) vertebrae, thirty-eight dorsal vertebrae (which includes thoracic and lumbar vertebrae) in the back, and eight pygal vertebrae (front tail vertebrae lacking haemal arches) followed by sixty-eight caudal vertebrae in the tail. All species of Mosasaurus have seven cervical vertebrae, but other vertebral counts vary among them. Various partial skeletons of M. conodon, M. hoffmannii, and M. missouriensis suggest M. conodon likely had up to thirty-six dorsal vertebrae and nine pygal vertebrae; M. hoffmannii had likely up to thirty-two dorsal vertebrae and ten pygal vertebrae; and M. missouriensis around thirty-three dorsal vertebrae, eleven pygal vertebrae, and at least seventy-nine caudal vertebrae. M. lemmonieri had the most vertebrae in the genus, with up to around forty dorsal vertebrae, twenty-two pygal vertebrae, and ninety caudal vertebrae. Compared to other mosasaurs, the rib cage of Mosasaurus is unusually deep and forms an almost perfect semicircle, giving it a barrel-shaped chest. Rather than being fused together, extensive cartilage likely connected the ribs with the sternum, which would have facilitated breathing movements and compression when in deeper waters. The texture of the bones is virtually identical with in modern whales, which indicates Mosasaurus possessed a high range of aquatic adaptation and neutral buoyancy as seen in cetaceans. The tail structure of Mosasaurus is similar to relatives like Prognathodon, in which soft tissue evidence for a two-lobed tail is known. The tail vertebrae gradually shorten around the center of the tail and lengthen behind the center, suggesting rigidness around the tail center and excellent flexibility behind it. Like most advanced mosasaurs, the tail bends slightly downwards as it approached the center, but this bend is offset from the dorsal plane at a small degree. Mosasaurus also has large haemal arches located at the bottom of each caudal vertebra which bend near the middle of the tail, which contrasts with the reduction of haemal arches in other marine reptiles such as ichthyosaurs. These and other features support a large and powerful paddle-like fluke in Mosasaurus.

The forelimbs of Mosasaurus are wide and robust. The scapula and humerus are fan-shaped and wider than tall. The radius and ulna are short, but the former is taller and larger than the latter. The ilium is rod-like and slender; in M. missouriensis, it is around 1.5 times longer than the femur. The femur itself is about twice as long as it is wide and ends at the distal side in a pair of distinct articular facets (of which one connects to the ilium and the other to the paddle bones) that meet at an angle of approximately 120°. Five sets of metacarpals and phalanges (finger bones) were encased in and supported the paddles, with the fifth set being shorter and offset from the rest. The overall structure of the paddle is compressed, similar to in Plotosaurus, and was well-suited for faster swimming. In the hindlimbs, the paddle is supported by four sets of digits.

Interactive skeletal reconstruction of M. hoffmannii

(hover over or click on each skeletal component to identify the structure)

History of taxonomy
Because nomenclatural rules were not well-defined at the time, 19th century scientists did not give Mosasaurus a proper diagnosis during its initial descriptions, which led to ambiguity in how the genus is defined. This led Mosasaurus to become a wastebasket taxon containing as many as fifty different species. A 2017 study by Hallie Street and Michael Caldwell performed the first proper diagnosis and description of the M. hoffmannii holotype, which allowed a major taxonomic cleanup confirming five species as likely valid—M. hoffmannii, M. missouriensis, M. conodon, M. lemonnieri, and M. beaugei. The study also held four additional species from Pacific deposits—M. mokoroa, M. hobetsuensis, M. flemingi, and M. prismaticus—to be possibly valid, pending a future formal reassessment. Street & Caldwell (2017) was derived from Street's 2016 doctoral thesis, which contained a phylogenetic study proposing the constraining of Mosasaurus into four species—M. hoffmannii, M. missouriensis, M. lemonnieri, and a proposed new species M. glycys—with M. conodon and the Pacific taxa belonging to different genera and M. beaugei being a synonym of M. hoffmannii.

Systematics and evolution
As the type genus of the family Mosasauridae and the subfamily Mosasaurinae, Mosasaurus is a member of the order Squamata (which comprises lizards and snakes). Relationships between mosasaurs and living squamates remain controversial as scientists still fiercely debate on whether the closest living relatives of mosasaurs are monitor lizards or snakes. Mosasaurus, along with mosasaur genera Eremiasaurus, Plotosaurus, and Moanasaurus traditionally form a tribe within the Mosasaurinae variously called Mosasaurini or Plotosaurini.

Phylogeny and evolution of the genus
One of the earliest relevant attempts at an evolutionary study of Mosasaurus was done by Russell in 1967. He proposed that Mosasaurus evolved from a Clidastes-like mosasaur, and diverged into two lineages, one giving rise to M. conodon and another siring a chronospecies sequence which contained in order of succession M. ivoensis, M. missouriensis, and M. maximus-hoffmanni. However, Russell used an early method of phylogenetics and did not use cladistics.

In 1997, Bell published the first cladistical study of North American mosasaurs. Incorporating the species M. missouriensis, M. conodon, M. maximus, and an indeterminate specimen (UNSM 77040), some of his findings agreed with Russell (1967), such as Mosasaurus descending from an ancestral group containing Clidastes and M. conodon being the most basal of the genus. Contrary to Russell (1967), Bell also recovered Mosasaurus in a sister relationship with another group which included Globidens and Prognathodon, and M. maximus as a sister species to Plotosaurus. The latter rendered Mosasaurus paraphyletic (an unnatural grouping), but Bell (1997) nevertheless recognized Plotosaurus as a distinct genus.

Bell's study served as a precedent for later studies that mostly left the systematics of Mosasaurus unchanged, although some later studies have recovered the sister group to Mosasaurus and Plotosaurus to instead be Eremiasaurus or Plesiotylosaurus depending on the method of data interpretation used,  with at least one study also recovering M. missouriensis to be the most basal species of the genus instead of M. conodon. In 2014, Konishi and colleagues expressed a number of concerns with the reliance on Bell's study. First, the genus was severely underrepresented by incorporating only the three North American species ''M. hoffmannii/M. maximus, M. missouriensis, and M. conodon; by doing so, others like M. lemonnieri'', which is one of the most completely known species in the genus, were neglected, which affected phylogenetic results. Second, the studies relied on an unclean and shaky taxonomy of the Mosasaurus genus due to the lack of a clear holotype diagnosis, which may have been behind the genus's paraphyletic status. Third, there was still a lack of comparative studies of the skeletal anatomy of large mosasaurines at the time. These problems were addressed in Street's 2016 thesis in an updated phylogenetic analysis.

Conrad uniquely used only M. hoffmannii and M. lemonnieri in his 2008 phylogenetic analysis, which recovered M. hoffmannii as basal to a multitude of descendant clades containing (in order of most to least basal) Globidens, M. lemonnieri, Goronyosaurus, and Plotosaurus. This result indicated that M. hoffmannii and M. lemonnieri are not in the same genus. However, the study used a method unorthodox to traditional phylogenetic studies on mosasaur species because its focus was on the relationships of entire squamate groups rather than mosasaur classification. As a result, some paleontologists caution that lower-order classification results from Conrad's 2008 study such as the specific placement of Mosasaurus may contain technical problems, making them inaccurate.

The following cladogram on the left (Topology A) is modified from a maximum clade credibility tree inferred by a Bayesian analysis in the most recent major phylogenetic analysis of the Mosasaurinae subfamily by Madzia & Cau (2017), which was self-described as a refinement of a larger study by Simões et al. (2017). The cladogram on the right (Topology B) is modified from Street's 2016 doctoral thesis proposing a revision to the Mosasaurinae, with proposed new taxa and renamings in single quotations.

Head musculature and mechanics
In 1995, Lingham-Soliar studied the head musculature of M. hoffmannii. Because soft tissue like muscles do not easily fossilize, reconstruction of the musculature was largely based on the structure of the skull, muscle scarring on the skull, and the musculature in extant monitor lizards.

In modern lizards, the mechanical build of the skull is characterized by a four-pivot geometric structure in the cranium that allows flexible movement of the jaws, possibly to allow the animals to better position them and prevent prey escape when hunting. In contrast, the frontal and parietal bones, which in modern lizards connect to form a flexible pivot point, overlap in the skull of M. hoffmannii. This creates a rigid three-pivot geometric cranial structure. These cranial structures are united by strong interlocking sutures formed to resist compression and shear forces caused by a downward thrust of the lower jaw muscles or an upward thrust of prey. This rigid but highly shock-absorbent structure of the cranium likely allowed a powerful bite force.

Like all mosasaurs, the lower jaws of Mosasaurus could swing forward and backward. In many mosasaurs like Prognathodon and M. lemonnieri, this function mainly served to allow ratchet feeding, in which the pterygoid and jaws would "walk" captured prey into the mouth like a conveyor belt. But especially compared to those in M. lemonnieri, the pterygoid teeth in M. hoffmannii are relatively small, which indicates ratchet feeding was relatively unimportant to its hunting and feeding. Rather, M. hoffmannii likely employed inertial feeding (in which the animal thrusts its head and neck backward to release a held prey item and immediately thrust the head and neck forward to close the jaws around the item ) and used jaw adduction to assist in biting during prey seizure. The magnus adductor muscles, which attach to the lower jaws to the cranium and have a major role in biting function, are massive, indicating M. hoffmannii was capable of enormous bite forces. The long, narrow, and heavy nature of the lower jaws and attachment of tendons at the coronoid process would have allowed quick opening and closing of the mouth with little energy input underwater, which also contributed to the powerful bite force of M. hoffmannii and suggests it would not have needed the strong magnus depressor muscles (jaw-opening muscles) seen in some plesiosaurs.

Mobility and thermoregulation
Mosasaurus swam using its tail. The swimming style was likely sub-carangiform, which is exemplified today by mackerels. Its elongated paddle-like limbs functioned as hydrofoils for maneuvering the animal. The paddles' steering function was enabled by large muscle attachments from the outwards-facing side of the humerus to the radius and ulna and modified joints allowed an enhanced ability of rotating the flippers. The powerful forces resulting from utilization of the paddles may have sometimes resulted in bone damage, as evidenced by a M. hoffmannii ilium with significant separation of the bone's head from the rest of the bone likely caused by frequent shearing forces at the articulation joint.

The tissue structure of Mosasaurus' bones suggests it had a metabolic rate much higher than modern squamates and its resting metabolic rate was between that of the leatherback sea turtle and that of ichthyosaurs and plesiosaurs. Mosasaurus was likely endothermic and maintained a constant body temperature independent of the external environment. Although there is no direct evidence specific to the genus, studies on the biochemistry of related mosasaur genera such as Clidastes suggests that endothermy was likely present in all mosasaurs. Such a trait is unique among squamates, the only known exception being the Argentine black and white tegu, which can maintain partial endothermy. This adaptation would have given several advantages to Mosasaurus, including increased stamina when foraging across larger areas and pursuing prey. It may have also been a factor that allowed Mosasaurus to thrive in the colder climates of locations such as Antarctica.

Sensory functions
Mosasaurus had relatively large eye sockets with large sclerotic rings occupying much of the sockets' diameter; the latter is correlated with eye size and suggests it had good vision. The eye sockets were located at the sides of the skull, which created a narrow field of binocular vision at around 28.5° but alternatively allowed excellent processing of a two-dimensional environment, such as the near-surface waters inhabited by Mosasaurus.

Brain casts made from fossils of Mosasaurus show that the olfactory bulb and vomeronasal organ, which both control the function of smell, are poorly developed and lack some structures in M. hoffmannii; this indicates the species had a poor sense of smell. In M. lemonnieri, these olfactory organs, although still small, are better developed and have some components lacking in M. hoffmannii. The lack of a strong sense of smell suggests that olfaction was not particularly important in Mosasaurus; instead, other senses like vision may have been more useful.

Feeding
Paleontologists generally agree that Mosasaurus was likely an active predator of a variety of marine animals. Fauna likely preyed upon by the genus include bony fish, sharks, cephalopods, birds, and marine reptiles such as other mosasaurs and turtles. It is unlikely Mosasaurus was a scavenger as it had a poor sense of smell. Mosasaurus was among the largest marine animals of its time, and with its large, robust cutting teeth, scientists believe larger members of the genus would have been able to handle virtually any animal. Lingham-Soliar (1995) suggested that Mosasaurus had a rather "savage" feeding behavior as demonstrated by large tooth marks on scutes of the giant sea turtle Allopleuron hoffmanni and fossils of re-healed fractured jaws in M. hoffmannii. The species likely hunted near the ocean surface as an ambush predator, using its large two-dimensionally adapted eyes to more effectively spot and capture prey. Chemical and structural data in the fossils of M. lemonnieri and M. conodon suggests they may have also hunted in deeper waters.

Carbon isotope studies on fossils of multiple M. hoffmannii individuals have found extremely low values of δ13C, the lowest in all mosasaurs for the largest individuals. Mosasaurs with lower δ13C values tended to occupy higher trophic levels, and one factor for this was dietary: a diet of prey rich in lipids such as sea turtles and other large marine reptiles can lower δ13C values. M. hoffmannii's low δ13C levels reinforces its likely position as an apex predator.

Currently, there is only one known example of a Mosasaurus preserved with stomach contents: a well-preserved partial skeleton of a small M. missouriensis dated about 75 million years old with dismembered and punctured remains of a 1 m long fish in its gut. This fish was much longer than the length of the mosasaur's skull, which measured 66 cm in length, confirming that M. missouriensis consumed prey larger than its head by dismembering and consuming bits at a time. Due to coexistence with other large mosasaurs like Prognathodon, which specialized in robust prey, M. missouriensis likely specialized more on prey best consumed using cutting-adapted teeth in an example of niche partitioning.

Mosasaurus may have taught their offspring how to hunt, as supported by a fossil nautiloid Argonautilus catarinae with bite marks from two conspecific mosasaurs, one being from a juvenile and the other being from an adult. Analysis of the tooth marks by a 2004 study by Kauffman concluded that the mosasaurs were either Mosasaurus or Platecarpus. The positioning of both bite marks are at the direction the nautiloid's head would have been facing, indicating it was incapable of escaping and was thus already sick or dead during the attacks; it is possible this phenomenon was from a parent mosasaur teaching its offspring about cephalopods as an alternate source of prey and how to hunt one. An alternate explanation postulates the bite marks as from one individual mosasaur that lightly bit the nautiloid at first, then proceeded to bite again with greater force. However, there are differences in tooth spacing between both bites which indicate different jaw sizes.

Intraspecific combat
There is fossil evidence that Mosasaurus engaged in aggressive and lethal combat with others of its kind. One partial skeleton of M. conodon bears multiple cuts, breaks, and punctures on various bones, particularly in the rear portions of the skull and neck, and a tooth from another M. conodon piercing through the quadrate bone. No injuries on the fossil show signs of healing, suggesting that the mosasaur was killed by its attacker by a fatal blow in the skull. Likewise, an M. missouriensis skeleton has a tooth from another M. missouriensis embedded in the lower jaw underneath the eye. In this case, there were signs of healing around the wound, implying survival of the incident. Takuya Konishi suggested an alternative cause of this example being head-biting behavior during courtship as seen in modern lizards. Attacks by another Mosasaurus are a possible cause of physical pathologies in other skulls, but they could have instead arisen from other incidents like attempted biting on hard turtle shells. In 2004, Lingham-Soliar observed that if these injuries were indeed the result of an intraspecific attack, then there is a pattern of them concentrating in the skull region. Modern crocodiles commonly attack each other by grappling an opponent's head using their jaws, and Lingham-Soliar hypothesized that Mosasaurus employed similar head-grappling behavior during intraspecific combat. Many of the fossils with injuries possibly attributable to intraspecific combat are of juvenile or sub-adult Mosasaurus, leading to the possibility that attacks on smaller, weaker individuals may have been more common. However, the attacking mosasaurs of the M. conodon and M. missouriensis specimens were likely similar in size to the victims. In 2006, Schulp and colleagues speculated that Mosasaurus may have occasionally engaged in cannibalism as a result of intraspecific aggression.

Diseases
There are some M. hoffmannii jaws with evidence of infectious diseases as a result of physical injuries. Two examples include IRSNB R25 and IRSNB R27, both having fractures and other pathologies in their dentaries. IRSNB R25 preserves a complete fracture near the sixth tooth socket. Extensive amounts of bony callus almost overgrowing the tooth socket are present around the fracture along with various osteolytic cavities, abscess canals, damages to the trigeminal nerve, and inflamed erosions signifying severe bacterial infection. There are two finely ulcerated scratches on the bone callus, which may have developed as part of the healing process. IRSNB R27 has two fractures: one had almost fully healed and the other is an open fracture with nearby teeth broken off as a result. The fracture is covered with a nonunion formation of bony callus with shallow scratch marks and a large pit connected to an abscess canal. Lingham-Soliar described this pit as resembling a tooth mark from a possible attacking mosasaur. Both specimens show signs of deep bacterial infection alongside the fractures; some bacteria may have spread to nearby damaged teeth and caused tooth decay, which may have entered deeper tissue from prior post-traumatic or secondary infections. The dentaries ahead of the fractures in both specimens are in good condition, suggesting that the arteries and trigeminal nerves had not been damaged; if they were, those areas would have necrotized due to lack of blood. The dentaries' condition suggests that the species may have had an efficient process of immobilizing the fracture during healing, which helped prevent damage to vital blood vessels and nerves. This, along with signs of healing, indicates that the fractures were not imminently fatal.

In 2006, Schulp and colleagues published a study describing a quadrate of M. hoffmannii with multiple unnatural openings and an estimated 0.5 L of tissue destroyed. This was likely a severe bone infection initiated by septic arthritis, which progressed to the point where a large portion of the quadrate was reduced to abscess. Extensive amounts of bone reparative tissue were also present, suggesting the infection and subsequent healing process may have progressed for a few months. This level of bone infection would have been tremendously painful and severely hampered the mosasaur's ability to use its jaws. The location of the infection may have also interfered with breathing. Considering how the individual was able to survive such conditions for an extended period of time, Schulp and colleagues speculated it switched to a foraging-type diet of soft-bodied prey like squid that could be swallowed whole to minimize jaw use. The cause of the infection remains unknown, but if it were a result of an intraspecific attack then it is possible one of the openings on the quadrate may have been the point of entry for an attacker's tooth from which the infection entered.

Avascular necrosis has been reported by many studies to be present in every examined specimen of M. lemonnieri and M. conodon. In examinations of M. conodon fossils from Alabama and New Jersey and M. lemonnieri fossils from Belgium, Rothschild and Martin in 2005 observed that the condition affected between 3-17% of the vertebrae in the mosasaurs' spines. Avascular necrosis is a common result of decompression illness; it involves bone damage caused by the formation of nitrogen bubbles from inhaled air decompressed during frequent deep-diving trips, or by intervals of repetitive diving and short breathing. This indicates that both Mosasaurus species may have either been habitual deep-divers or repetitive divers. Agnete Weinreich Carlsen considered it the simplest explanation that such conditions were a product of inadequate anatomical adaptation. Nevertheless, fossils of other mosasaurs with invariable avascular necrosis still exhibit substantial adaptations like eardrums that were well-protected from rapid changes in pressure.

Unnatural fusion of tail vertebrae has been documented in Mosasaurus, which occurs when the bones remodel themselves after damage from trauma or disease. A 2015 study by Rothschild and Everhart surveyed 15 Mosasaurus specimens from North America and Belgium and found cases of fused tail vertebrae in three of them. Two of these cases displayed irregular surface deformities around the fusion site caused by drainage of the vertebral sinuses, which is indicative of a bone infection. The causes of such infections are uncertain, but records of fused vertebrae in other mosasaurs suggest attacks by sharks and other predators as a possible candidate. The third case was determined to be caused by a form of arthritis based on the formation of smooth bridging between fused vertebrae.

Life history
It is likely that Mosasaurus was viviparous (giving live birth) like most modern mammals today. There is no evidence for live birth in Mosasaurus itself, but it is known in a number of other mosasaurs; examples include a skeleton of a pregnant Carsosaurus, a Plioplatecarpus fossil associated with fossils of two mosasaur embryos, and fossils of newborn Clidastes from pelagic (open ocean) deposits. Such fossil records, along with a total absence of any evidence suggesting external egg-based reproduction, indicates the likeliness of viviparity in Mosasaurus. Microanatomical studies on bones of juvenile Mosasaurus and related genera have found that their bone structures are comparable to adults. They do not exhibit the bone mass increase found in juvenile primitive mosasauroids to support buoyancy associated with a lifestyle in shallow water, implying that Mosasaurus was precocial: they were already efficient swimmers and lived fully functional lifestyles in open water at a very young age, and did not require nursery areas to raise their young. Some areas in Europe and South Dakota have yielded concentrated assemblages of juvenile M. hoffmannii, M. missouriensis and/or M. lemonnieri. These localities are all shallow ocean deposits, suggesting that juvenile Mosasaurus may still have lived in shallow waters.

Distribution, ecosystem, and ecological impact
Mosasaurus had a transatlantic distribution, with its fossils having been found in marine deposits on both sides of the Atlantic Ocean. These localities include the Midwest and East Coast of the United States, Canada, Europe, Turkey, Russia, the Levant, the African coastline from Morocco to South Africa, Brazil, Argentina, and Antarctica. During the Late Cretaceous, these regions made up the three seaways inhabited by Mosasaurus: the Atlantic Ocean, the Western Interior Seaway, and the Mediterranean Tethys. Multiple oceanic climate zones encompassed the seaways, including tropical, subtropical, temperate, and subpolar climates. The wide range of oceanic climates yielded a large diversity of fauna that coexisted with Mosasaurus.

Mediterranean Tethys
The Mediterranean Tethys during the Maastrichtian stage was located in what is now Europe, Africa, and the Middle East. In recent studies, the confirmation of paleogeographical affinities extended this range to areas across the Atlantic including Brazil and the East Coast state of New Jersey. It is geographically subdivided into two biogeographic provinces that respectively include the northern and southern Tethyan margins. The two mosasaurs Mosasaurus and Prognathodon appear to have been the dominant taxa, being widespread and ecologically diversified throughout the seaway.

The northern Tethyan margin was located around the paleolatitudes of 30–40°N, consisting of what is now the European continent, Turkey, and New Jersey. At the time, Europe was a scattering of islands with most of the modern continental landmass being underwater. The margin provided a warm-temperate climate with habitats dominated by mosasaurs and sea turtles. M. hoffmannii and Prognathodon sectorius were the dominant species in the northern province. In certain areas such as Belgium, other Mosasaurus species like M. lemonnieri were instead the dominant species, where its occurrences greatly outnumber those of other large mosasaurs. Other mosasaurs found in the European side of the northern Tethyan margin include smaller genera such as Halisaurus, Plioplatecarpus, and Platecarpus; the shell-crusher Carinodens; and larger mosasaurs of similar trophic levels including Tylosaurus bernardi and four other species of Prognathodon. Sea turtles such as Allopleurodon hoffmanni and Glyptochelone suickerbuycki were also prevalent in the area and other marine reptiles including indeterminate elasmosaurs have been occasionally found. Marine reptile assemblages in the New Jersey region of the province are generally equivalent with those in Europe; the mosasaur faunae are quite similar but exclude M. lemonnieri, Carinodens, Tylosaurus, and certain species of Halisaurus and Prognathodon. In addition, they exclusively feature M. conodon, Halisaurus platyspondylus and Prognathodon rapax. Many types of sharks such as Squalicorax, Cretalamna, Serratolamna, and sand sharks, as well as bony fish such as Cimolichthys, the saber-toothed herring Enchodus, and the swordfish-like Protosphyraena are represented in the northern Tethyan margin.

The southern Tethyan margin was located along the equator between 20°N and 20°S, resulting in warmer tropical climates. Seabeds bordering the cratons in Africa and Arabia and extending to the Levant and Brazil provided vast shallow marine environments. These environments were dominated by mosasaurs and marine side-necked turtles. Of the mosasaurs, Globidens phosphaticus is the characteristic species of the southern province; in the African and Arabian domain, Halisaurus arambourgi and Platecarpus ptychodon were also common mosasaurs alongside Globidens. Mosasaurus was not well-represented: the distribution of M. beaugei was restricted to Morocco and Brazil and isolated teeth from Syria suggested a possible presence of M. lemonnieri, although M. hoffmannii also had some presence throughout the province. Other mosasaurs from the southern Tethyan margin include the enigmatic Goronyosaurus, the shell-crushers Igdamanosaurus and Carinodens, Eremiasaurus, four other species of Prognathodon, and various other species of Halisaurus. Other marine reptiles such as the marine monitor lizard Pachyvaranus and the sea snake Palaeophis are known there. Aside from Zarafasaura in Morocco, plesiosaurs were scarce. As a tropical area, bony fish such as Enchodus and Stratodus and various sharks were common throughout the southern Tethyan margin.

Western Interior Seaway
Many of the earliest fossils of Mosasaurus were found in Campanian stage deposits in North America, including the Western Interior Seaway, an inland sea which once flowed through what is now the central United States and Canada, and connected the Arctic Ocean to the modern-day Gulf of Mexico. The region was shallow for a seaway, reaching a maximum depth of about 800-900 m. Extensive drainage from the neighboring continents, Appalachia and Laramidia, brought in vast amounts of sediment. Together with the formation of a nutrient-rich deepwater mass from the mixing of continental freshwater, Arctic waters from the north, and warmer saline Tethyan waters from the south, this created a warm and productive seaway that supported a rich diversity of marine life.

The biogeography of the region has been subdivided into two Interior Subprovinces characterized by different climates and faunal structures, and their borders are separated in modern-day Kansas. The oceanic climate of the Northern Interior Subprovince was likely a cool temperate one, while the Southern Interior Subprovince had warm temperate to subtropical climates. The fossil assemblages throughout these regions suggest a complete faunal turnover when M. missouriensis and M. conodon appeared at 79.5 Ma, indicating that the presence of Mosasaurus in the Western Interior Seaway had a profound impact on the restructuring of marine ecosystems. The faunal structure of both provinces was generally much more diverse prior to the appearance of Mosasaurus, during a faunal stage known as the Niobraran Age, than it was during the following Navesinkan Age.

In what is now Alabama within the Southern Interior Subprovince, most of the key genera including sharks like Cretoxyrhina and the mosasaurs Clidastes, Tylosaurus, Globidens, Halisaurus, and Platecarpus disappeared and were replaced by Mosasaurus. During the Navesinkan Age, Mosasaurus dominated the whole region, accounting for around two-thirds of all mosasaur diversity with Plioplatecarpus and Prognathodon sharing the remaining third. The Northern Interior Subprovince also saw a restructuring of mosasaur assemblages, characterized by the disappearance of mosasaurs like Platecarpus and their replacement by Mosasaurus and Plioplatecarpus. Some Niobraran genera such as Tylosaurus, Cretoxyrhina, hesperornithids, and plesiosaurs including elasmosaurs such as Terminonatator and polycotylids like Dolichorhynchops maintained their presence until around the end of the Campanian, during which the entire Western Interior Seaway started receding from the north. Mosasaurus continued to be the dominant genus in the seaway until the end of the Navesinkan Age at the end of the Cretaceous. Contemporaneous fauna included sea turtles such as Protostega and Archelon; many species of sea birds including Baptornis, Ichthyornis, and Halimornis; sharks such as the mackerel sharks Cretalamna, Squalicorax, Pseudocorax, and Serratolamna, the goblin shark Scapanorhynchus, the sand tiger Odontaspis, and the sawfish-like Ischyrhiza; and bony fish such as Enchodus, Protosphyraena, Stratodus, and the ichthyodectids Xiphactinus and Saurodon.

Antarctica
Mosasaurus is known from late Maastrichtian deposits in the Antarctic Peninsula, specifically the López de Bertodano Formation in Seymour Island. Located within the polar circle at around 65°S, temperatures at medium to large water depths would have been around 6 C on average, while sea surface temperatures may have dropped below freezing and sea ice may have formed at times. Mosasaurus appears to be the most diverse mosasaur in the Maastrichtian Antarctica. At least two species of Mosasaurus have been described, but the true number of species is unknown as remains are often fragmentary and specimens are described in open nomenclature. These species include one comparable with M. lemonnieri, and another that appears to be closely related to M. hoffmannii. M. sp. has also been described. However, it is possible that such specimens may actually represent Moanasaurus, although this depends on the outcome of a pending revision of the genus. At least four other mosasaur genera have been reported in Antarctica, including Plioplatecarpus, the mosasaurines Moanasaurus and Liodon, and Kaikaifilu. The validity of some of these genera is disputed as they are primarily based on isolated teeth. Prognathodon and Globidens are also expected to be present based on distribution trends of both genera, although conclusive fossils have yet to be found. Other Antarctic marine reptiles included elasmosaurid plesiosaurs like Aristonectes and another indeterminate elasmosaurid. The fish assemblage of the López de Bertodano Formation was dominated by Enchodus and ichthyodectiformes.

Habitat preference
Known fossils of Mosasaurus have typically been recovered from deposits representing nearshore habitats during the Cretaceous period, with some fossils coming from deeper-water deposits. Lingham-Soliar (1995) elaborated on this, finding that Maastrichtian deposits in the Netherlands with M. hoffmannii occurrences represented nearshore waters around 40-50 m deep. Changing temperatures and an abundance in marine life were characteristic of these localities. The morphological build of M. hoffmannii, nevertheless, was best adapted for a pelagic surface lifestyle.

δ13C is also correlated with a marine animal's feeding habitat as isotope levels deplete when habitat is farther from the shoreline, so some scientists interpreted isotope levels as a proxy for habitat preference. Separate studies involving multiple Mosasaurus specimens have yielded consistently low δ13C levels of tooth enamel, indicating that Mosasaurus fed in more offshore or open waters. It has been pointed out how δ13C can be influenced by other factors in an animal's lifestyle, such as diet and diving behavior. To account for this, a 2014 study by T. Lynn Harrell Jr. and Alberto Perez-Huerta examined the concentration ratios of neodymium, gadolinium, and ytterbium in M. hoffmannii and Mosasaurus sp. fossils from Alabama, the Demopolis Chalk, and the Hornerstown Formation. Previous studies demonstrated that ratios of these three elements can act as a proxy for relative ocean depth of a fossil during early diagenesis without interference from biological processes, with each of the three elements signifying either shallow, deep, or fresh waters. The rare earth element ratios were very consistent throughout most of the examined Mosasaurus fossils, indicating consistent habitat preference, and clustered towards a ratio representing offshore habitats with ocean depths deeper than 50 m.

Interspecific competition
Mosasaurus lived alongside other large predatory mosasaurs also considered apex predators, most prominent among them being the tylosaurines and Prognathodon. Tylosaurus bernardi, the only surviving species of the genus during the Maastrichtian, measured up to 12.2 m in length while the largest coexisting species of Prognathodon like P. saturator exceeded 12 m. These three mosasaurs preyed on similar animals such as marine reptiles.

A study published in 2013 by Schulp and colleagues specifically tested how mosasaurs such as M. hoffmannii and P. saturator were able to coexist in the same localities through δ13C analysis. The scientists utilized an interpretation that differences in isotope values can help explain the level of resource partitioning because it is influenced by multiple environmental factors such as lifestyle, diet, and habitat preference. Comparisons between the δ13C levels in multiple teeth of M. hoffmannii and P. saturator from the Maastrichtian-age Maastricht Formation showed that while there was some convergence between certain specimens, the average δ13C values between the two species were on average different. This is one indication of niche partitioning, where the two mosasaur genera likely foraged in different habitats or had different specific diets to coexist without direct competitive conflict. The teeth of P. saturator are much more robust than those of M. hoffmannii and were specifically equipped for preying on robust prey like turtles. While M. hoffmannii also preyed on turtles, its teeth were built to handle a wider range of prey less suited for P. saturator.

Another case of presumed niche partitioning between Mosasaurus and Prognathodon from the Bearpaw Formation in Alberta was documented in a 2014 study by Konishi and colleagues. The study found a dietary divide between M. missouriensis and Prognathodon overtoni based on stomach contents. Stomach contents of P. overtoni included turtles and ammonites, providing another example of a diet specialized for harder prey. In contrast, M. missouriensis had stomach contents consisting of fish, indicative of a diet specialized in softer prey. It was hypothesized that these adaptations helped maintain resource partitioning between the two mosasaurs.

Nevertheless, competitive engagement evidently could not be entirely avoided. There is also evidence of aggressive interspecific combat between Mosasaurus and other large mosasaur species. This is shown from a fossil skull of a subadult M. hoffmannii with fractures caused by a massive concentrated blow to the braincase; Lingham-Soliar (1998) argued that this blow was dealt by a ramming attack by Tylosaurus bernardi, as the formation of the fractures were characteristic of a coordinated strike (and not an accident or fossilization damage), and T. bernardi was the only known coexisting animal likely capable of causing such damage, using its robust arrow-like elongated snout. This sort of attack has been compared to the defensive behavior of bottlenose dolphins using their beaks to kill or repel lemon sharks, and it has been speculated that T. bernardi dealt the offensive attack via an ambush on an unsuspecting Mosasaurus.

Extinction
By the end of the Cretaceous, mosasaurs were at the height of their evolutionary radiation, and their extinction was a sudden event. During the late Maastrichtian, global sea levels dropped, draining the continents of their nutrient-rich seaways and altering circulation and nutrient patterns, and reducing the number of available habitats for Mosasaurus. The genus adapted by accessing new habitats in more open waters. The last fossils of Mosasaurus, which include those of M. hoffmannii and indeterminate species, occur up to the Cretaceous-Paleogene boundary (K-Pg boundary). The demise of the genus was likely a result of the Cretaceous-Paleogene extinction event which also wiped out the non-avian dinosaurs. Mosasaurus fossils have been found less than 15 m below the boundary in the Maastricht Formation, the Davutlar Formation in Turkey, the Jagüel Formation in Argentina, Stevns Klint in Denmark, Seymour Island, and Missouri.

M. hoffmannii fossils have been found within the K-Pg boundary itself in southeastern Missouri between the Paleocene Clayton Formation and Cretaceous Owl Creek Formation. Fossil vertebrae from the layer were found with fractures formed after death. The layer was likely deposited as a tsunamite, alternatively nicknamed the "Cretaceous cocktail deposit". This formed through a combination of catastrophic seismic and geological disturbances, mega-hurricanes, and giant tsunamis caused by the impact of the Chicxulub asteroid that catalyzed the K-Pg extinction event. As well as physical destruction, the impact also blocked out sunlight leading to a collapse of marine food webs. Any Mosasaurus surviving the immediate cataclysms by taking refuge in deeper waters would have died out due to starvation from a loss of prey.

One enigmatic occurrence of Mosasaurus sp. fossils is in the Hornerstown Formation, a deposit typically dated to be from the Paleocene Danian age, which was immediately after the Maastrichtian age. The fossils were found in association with fossils of Squalicorax, Enchodus, and various ammonites within a uniquely fossil-rich bed at the base of the Hornerstown Formation known as the Main Fossiliferous Layer. This does not mean Mosasaurus and its associated fauna survived the K-Pg extinction. According to one hypothesis, the fossils may have originated from an earlier Cretaceous deposit and were reworked into the Paleocene formation during its early deposition. Evidence of reworking typically comes from fossils worn down due to further erosion during their exposure at the time of redeposition. Many of the Mosasaurus fossils from the Main Fossiliferous Layer consist of isolated bones commonly abraded and worn, but the layer also yielded better-preserved Mosasaurus remains. Another explanation suggests the Main Fossiliferous Layer is a Maastrichtian time-averaged remanié deposit, which means it originated from a Cretaceous deposit with winnowed low-sediment conditions. A third hypothesis proposes that the layer is a lag deposit of Cretaceous sediments forced out by a strong impact by a tsunami, and what remained was subsequently refilled with Cenozoic fossils.

title: Mosasaurus


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User:Maarbellecann

marbellecann

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User talk:Maliyjandro

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User:Sirfrummel

Hi, I'm David Kedron. I'm 32 and I live in Grand Rapids, MI.

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User talk:LandoSr

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Lord Armstrong

Lord Armstrong may refer to:
 * Iain Armstrong, Lord Armstrong (born 1956), Senator of the College of Justice in Scotland
 * Robert Armstrong, Baron Armstrong of Ilminster (1927–2020), British former civil servant
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 * William Armstrong, 1st Baron Armstrong (1810–1900)
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 * William Watson-Armstrong, 3rd Baron Armstrong (1919–1987)

title: Lord Armstrong