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• W2100240151 endingPage "317" @default.
• W2100240151 startingPage "299" @default.
• W2100240151 abstract "The late Campanian–Maastrichtian Liscomb Bonebed is the richest source of dinosaur remains thus far documented in the polar regions. This bed is formally defined herein and assigned to the upper part of the Prince Creek Formation; the bonebed and several other organic-rich beds are part of a 178 m sequence of fluvial and volcaniclastic deposits. The Liscomb Bonebed is a mudstone rich in clay, comminuted plant remains, and palynomorphs with a total organic carbon (TOC) of 6.80%–10.55%. It contains a multitaxic, low-diversity, dinosaur assemblage, dominated by Edmontosaurus sp., which is primarily represented by late juveniles. Four theropod taxa are almost exclusively represented by isolated teeth. With >6000 specimens collected, the assemblage is characterized by a Minimum Number of Individuals (MNI) of 36, dominance of Voorhies Groups I and II, and an underrepresentation of teeth, skulls, and girdles. Bones are highly fragmented and exhibit low weathering and abrasion indices. Bite marks occur on slightly more than 1% of elements. The densest accumulations of bone are typically found in the middle third of the bed with the largest bones at the bottom. The Liscomb Bonebed assemblage resulted from mass mortality associated with overbank floods that formed floodplain mires and ponds. Data from the current study clearly establish the Alaskan Arctic as the year-round residence of a rich dinosaur fauna and add further support to the hypotheses that even high-latitude hadrosaurids were gregarious and formed social groups." @default.
• W2100240151 created "2016-06-24" @default.
• W2100240151 creator A5007990431 @default.
• W2100240151 creator A5079830572 @default.
• W2100240151 date "2010-05-01" @default.
• W2100240151 modified "2023-10-12" @default.
• W2100240151 title "TAPHONOMY AND PALEOECOLOGY OF A BONEBED FROM THE PRINCE CREEK FORMATION, NORTH SLOPE, ALASKA" @default.
• W2100240151 cites W107722960 @default.
• W2100240151 cites W124955433 @default.
• W2100240151 cites W1491928515 @default.
• W2100240151 cites W1509986448 @default.
• W2100240151 cites W1541594191 @default.
• W2100240151 cites W158108064 @default.
• W2100240151 cites W1587340106 @default.
• W2100240151 cites W1630322587 @default.
• W2100240151 cites W1963182833 @default.
• W2100240151 cites W1967697037 @default.
• W2100240151 cites W1968223875 @default.
• W2100240151 cites W1970136096 @default.
• W2100240151 cites W1980591869 @default.
• W2100240151 cites W1981553904 @default.
• W2100240151 cites W1988961745 @default.
• W2100240151 cites W1992839242 @default.
• W2100240151 cites W199413854 @default.
• W2100240151 cites W2001396577 @default.
• W2100240151 cites W2002323615 @default.
• W2100240151 cites W2006585985 @default.
• W2100240151 cites W2020442186 @default.
• W2100240151 cites W2024771330 @default.
• W2100240151 cites W2033873112 @default.
• W2100240151 cites W2035411844 @default.
• W2100240151 cites W2036224036 @default.
• W2100240151 cites W2042338894 @default.
• W2100240151 cites W2042788701 @default.
• W2100240151 cites W2048344710 @default.
• W2100240151 cites W2055060023 @default.
• W2100240151 cites W2056724064 @default.
• W2100240151 cites W2058295360 @default.
• W2100240151 cites W2068650132 @default.
• W2100240151 cites W2073535777 @default.
• W2100240151 cites W2075814369 @default.
• W2100240151 cites W2082891696 @default.
• W2100240151 cites W2083771757 @default.
• W2100240151 cites W2085100494 @default.
• W2100240151 cites W2085377090 @default.
• W2100240151 cites W2085905171 @default.
• W2100240151 cites W2089282094 @default.
• W2100240151 cites W2089648191 @default.
• W2100240151 cites W2090426713 @default.
• W2100240151 cites W2102812357 @default.
• W2100240151 cites W2108271456 @default.
• W2100240151 cites W2124385948 @default.
• W2100240151 cites W2131530018 @default.
• W2100240151 cites W2140928384 @default.
• W2100240151 cites W2142364154 @default.
• W2100240151 cites W2153225664 @default.
• W2100240151 cites W2159630773 @default.
• W2100240151 cites W2161105980 @default.
• W2100240151 cites W2176916342 @default.
• W2100240151 cites W2179073245 @default.
• W2100240151 cites W2179225693 @default.
• W2100240151 cites W2180731239 @default.
• W2100240151 cites W2183707334 @default.
• W2100240151 cites W2190414927 @default.
• W2100240151 cites W2197414505 @default.
• W2100240151 cites W2199689614 @default.
• W2100240151 cites W2239754916 @default.
• W2100240151 cites W2284824064 @default.
• W2100240151 cites W2317865496 @default.
• W2100240151 cites W2323263299 @default.
• W2100240151 cites W2323485721 @default.
• W2100240151 cites W2330502294 @default.
• W2100240151 cites W2337457383 @default.
• W2100240151 cites W2338356952 @default.
• W2100240151 cites W2343378821 @default.
• W2100240151 cites W2343476843 @default.
• W2100240151 cites W2414228683 @default.
• W2100240151 cites W2484718763 @default.
• W2100240151 cites W2495255272 @default.
• W2100240151 cites W2504980750 @default.
• W2100240151 cites W2562157182 @default.
• W2100240151 cites W2604993090 @default.
• W2100240151 cites W2797576364 @default.
• W2100240151 cites W2910978022 @default.
• W2100240151 cites W2989049194 @default.
• W2100240151 cites W5048998 @default.
• W2100240151 cites W562380730 @default.
• W2100240151 cites W580652914 @default.
• W2100240151 cites W597250316 @default.
• W2100240151 cites W604333344 @default.
• W2100240151 cites W647458292 @default.
• W2100240151 cites W648608256 @default.
• W2100240151 cites W795479545 @default.
• W2100240151 cites W98190324 @default.
• W2100240151 cites W597685939 @default.
• W2100240151 doi "https://doi.org/10.2110/palo.2009.p09-103r" @default.
• W2100240151 hasPublicationYear "2010" @default.
• W2100240151 type Work @default.

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