A new earliest Paleocene (Puercan) mammalian fauna from Colorado's Denver Basin, U.S.A.

Q3 Earth and Planetary Sciences Rocky Mountain Geology Pub Date : 2016-01-01 DOI:10.2113/GSROCKY.51.1.1
E. L. Dahlberg, J. Eberle, J. Sertich, I. Miller
{"title":"A new earliest Paleocene (Puercan) mammalian fauna from Colorado's Denver Basin, U.S.A.","authors":"E. L. Dahlberg, J. Eberle, J. Sertich, I. Miller","doi":"10.2113/GSROCKY.51.1.1","DOIUrl":null,"url":null,"abstract":"Few areas preserve the Cretaceous–Paleogene (K–Pg) boundary and earliest Paleocene (Puercan) mammalian faunas better than Colorado9s Denver Basin. Research conducted decades ago described a diverse Puercan fauna from the Denver Basin, but many would agree that the best-known fauna in the basin—the Littleton fauna—probably represents a late early-Puercan (i.e., late Pu1) assemblage. Renewed collecting of fossil mammals from Denver Museum of Nature & Science (DMNH) loc. 2560 in the Denver Formation on the eastern side of the Denver Basin—approximately nine meters stratigraphically above the K–Pg boundary—has produced a Puercan faunal assemblage containing isolated teeth of at least nine species of fossil mammal. Based upon its faunal composition, low diversity, absence of taxa characteristic of middle and late Puercan faunal assemblages, and close stratigraphic proximity to the K–Pg boundary, the fauna from DMNH loc. 2560 probably represents a Puercan fauna that is earlier than the Littleton fauna. It is most similar to early Puercan (Pu1) faunas in Wyoming and northeast Montana. We document the occurrence of three species of the multituberculate Mesodma ( M. ambigua, M. formosa , and M. hensleighi ), the cimolodont Cimexomys minor , the marsupial Thylacodon montanensis , and four species of archaic ungulate (or ‘condylarth’), including Protungulatum donnae , Oxyprimus sp., Baioconodon nordicus , and Maiorana sp. The presence of P. donnae defines the onset of the Puercan age, while Oxyprimus, Maiorana , and B. nordicus are restricted elsewhere to Pu1. C. minor is known from Lancian and early Puercan (Pu1) localities. The faunal assemblage from DMNH loc. 2560 indicates that the characteristic, low-diversity Pu1 fauna found in Montana and Wyoming extended as far south as Colorado. Additionally, we report the occurrence of the ‘condylarth’ Ampliconus browni from the South Table Mountain locality (DHMH loc. 2814) near Golden, Colorado. Its presence corroborates research by others that this locality is probably temporally correlative to the late early-Puercan (late Pu1) Alexander locality south of Denver, Colorado (UCM loc. 77267 [UCM = University of Colorado Museum of Natural History]). Our research provides a more complete picture of early Puercan mammalian diversity in the Denver Basin and a means to temporally correlate early Puercan faunas from Montana to Colorado.","PeriodicalId":34958,"journal":{"name":"Rocky Mountain Geology","volume":"51 1","pages":"1-22"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.2113/GSROCKY.51.1.1","citationCount":"14","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Rocky Mountain Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2113/GSROCKY.51.1.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 14

Abstract

Few areas preserve the Cretaceous–Paleogene (K–Pg) boundary and earliest Paleocene (Puercan) mammalian faunas better than Colorado9s Denver Basin. Research conducted decades ago described a diverse Puercan fauna from the Denver Basin, but many would agree that the best-known fauna in the basin—the Littleton fauna—probably represents a late early-Puercan (i.e., late Pu1) assemblage. Renewed collecting of fossil mammals from Denver Museum of Nature & Science (DMNH) loc. 2560 in the Denver Formation on the eastern side of the Denver Basin—approximately nine meters stratigraphically above the K–Pg boundary—has produced a Puercan faunal assemblage containing isolated teeth of at least nine species of fossil mammal. Based upon its faunal composition, low diversity, absence of taxa characteristic of middle and late Puercan faunal assemblages, and close stratigraphic proximity to the K–Pg boundary, the fauna from DMNH loc. 2560 probably represents a Puercan fauna that is earlier than the Littleton fauna. It is most similar to early Puercan (Pu1) faunas in Wyoming and northeast Montana. We document the occurrence of three species of the multituberculate Mesodma ( M. ambigua, M. formosa , and M. hensleighi ), the cimolodont Cimexomys minor , the marsupial Thylacodon montanensis , and four species of archaic ungulate (or ‘condylarth’), including Protungulatum donnae , Oxyprimus sp., Baioconodon nordicus , and Maiorana sp. The presence of P. donnae defines the onset of the Puercan age, while Oxyprimus, Maiorana , and B. nordicus are restricted elsewhere to Pu1. C. minor is known from Lancian and early Puercan (Pu1) localities. The faunal assemblage from DMNH loc. 2560 indicates that the characteristic, low-diversity Pu1 fauna found in Montana and Wyoming extended as far south as Colorado. Additionally, we report the occurrence of the ‘condylarth’ Ampliconus browni from the South Table Mountain locality (DHMH loc. 2814) near Golden, Colorado. Its presence corroborates research by others that this locality is probably temporally correlative to the late early-Puercan (late Pu1) Alexander locality south of Denver, Colorado (UCM loc. 77267 [UCM = University of Colorado Museum of Natural History]). Our research provides a more complete picture of early Puercan mammalian diversity in the Denver Basin and a means to temporally correlate early Puercan faunas from Montana to Colorado.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
美国科罗拉多州丹佛盆地发现的一种新的最早的古新世哺乳动物群
科罗拉多丹佛盆地是保存白垩纪-古近纪(K-Pg)界线和最早古新世(Puercan)哺乳动物群最好的地区。几十年前进行的研究描述了丹佛盆地的多种普尔坎动物群,但许多人都同意,该盆地最著名的动物群——利特尔顿动物群——可能代表了普尔坎晚期(即普尔坎晚期)的组合。从丹佛自然与科学博物馆(DMNH)重新收集哺乳动物化石。在丹佛盆地东侧的丹佛组2560,在K-Pg边界上大约9米的地层上,已经产生了一个普尔坎动物群,其中包含至少9种化石哺乳动物的分离牙齿。根据其区系组成、多样性低、缺乏普尔坎中晚期区系组合特征以及地层接近K-Pg边界的特点,推测其区系属于DMNH区系。2560可能代表一个比Littleton动物群更早的Puercan动物群。它与怀俄明州和蒙大拿州东北部的早期普尔坎(Pu1)动物群最相似。我们记录了三种多瘤的Mesodma (M. ambigua, M. formosa和M. hensleighi), cimolodon Cimexomys minor,有袋类Thylacodon montanensis,以及四种古代有蹄动物(或“尖齿动物”),包括Protungulatum donnae, Oxyprimus sp., Baioconodon nordicus和Maiorana sp.。P. donnae的存在定义了Puercan时代的开始,而Oxyprimus, Maiorana和B. nordicus仅限于Pu1。小c在兰西亚和早期普尔坎(Pu1)地区已知。DMNH地区的动物群。2560表明,在蒙大拿州和怀俄明州发现的具有特色的、低多样性的Pu1动物群一直向南延伸到科罗拉多州。此外,我们还报道了在南桌山地区(DHMH loc)发现的“髁缘”Ampliconus browni。2814)科罗拉多州戈尔登附近。它的存在证实了其他人的研究,即这个地方可能在时间上与科罗拉多州丹佛南部(UCM loc)的普尔坎(Pu1晚期)亚历山大(Alexander)地区相关。77267 [UCM =科罗拉多大学自然历史博物馆])。我们的研究为丹佛盆地早期普尔坎哺乳动物多样性提供了一个更完整的图景,并为从蒙大拿州到科罗拉多州的早期普尔坎动物群提供了一种时间相关性的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Rocky Mountain Geology
Rocky Mountain Geology Earth and Planetary Sciences-Geology
CiteScore
1.10
自引率
0.00%
发文量
4
期刊介绍: Rocky Mountain Geology (formerly Contributions to Geology) is published twice yearly by the Department of Geology and Geophysics at the University of Wyoming. The focus of the journal is regional geology and paleontology of the Rocky Mountains and adjacent areas of western North America. This high-impact, scholarly journal, is an important resource for professional earth scientists. The high-quality, refereed articles report original research by top specialists in all aspects of geology and paleontology in the greater Rocky Mountain region.
期刊最新文献
The edge of a Permian erg: Eolian facies and provenance of the Lyons Sandstone in northern Colorado U–Pb zircon ages, mapping, and biostratigraphy of the Payette Formation and Idaho Group north of the western Snake River Plain, Idaho: Implications for hydrocarbon system correlation Palynology of Permian red-bed successions of Colorado and Wyoming and its influence on Laramide strata A record of Late Jurassic vertebrates from Texas Recurrent fill history of individual clastic dikes in the White River Group at Slim Buttes, South Dakota
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1