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Mammals from the earliest Uintan (middle Eocene) Turtle Bluff Member, Bridger Formation, southwestern Wyoming, USA, Part 3: Marsupialia and a reevaluation of the Bridgerian-Uintan North American Land Mammal Age transition
被引:8
|作者:
Murphey, Paul C.
[1
]
Kelly, Thomas S.
[2
]
Chamberlain, Kevin R.
[3
,4
]
Tsukui, Kaori
[5
]
Clyde, William C.
[6
]
机构:
[1] San Diego Museum Nat Hist, Dept Paleontol, 1788 El Prado, San Diego, CA 92101 USA
[2] Nat Hist Museum Angeles Cty, Vertebrate Paleontol Dept, 900 Exposit Blvd, Los Angeles, CA 90007 USA
[3] Univ Wyoming, Dept Geol & Geophys, 1000 E Univ Ave, Laramie, WY 82071 USA
[4] Tomsk State Univ, Fac Geol & Geog, Tomsk 634050, Russia
[5] MIT, Dept Earth Atmospher & Planetary Sci, 77 Massachusetts Ave, Cambridge, MA 02139 USA
[6] Univ New Hampshire, Dept Earth Sci, 56 Coll Rd, Durham, NH 03824 USA
关键词:
biostratigraphy;
Eocene;
Marsupialia;
Uintan;
magnetostratigraphy;
U-Pb dating;
GREEN RIVER FORMATION;
CREEK LOCAL FAUNA;
U-PB;
ASTRONOMICAL CALIBRATION;
DECAY CONSTANTS;
GEOCHRONOLOGY;
HERPETOTHERIUM;
TERTIARY;
ZIRCON;
PALEOMAGNETISM;
D O I:
10.26879/804
中图分类号:
Q91 [古生物学];
学科分类号:
0709 ;
070903 ;
摘要:
This is the third and last of a series of reports that provide detailed descriptions and taxonomic revisions of the fauna from the Turtle Bluff Member (TBM) of the middle Eocene Bridger Formation of southwestern Wyoming. The TBM has been designated as the stratotype section for biochron Ui1a (earliest Uintan) of the Uintan North American Land Mammal age and here we document new faunal elements along with new UPb geochronologic and paleomagnetic data for the TBM. Prior to these reports, detailed systematic accounts of the taxa from the TBM were unavailable with the exception of one primate (Hemiacodon engardae). Here we document the occurrence of the following didelphimorphian marsupials from the TBM: Herpetotherium knighti, Herpetotherium marsupium, Peradectes chesteri, and Peradectes californicus. New UPb dates of 47.31 +/- 0.06 Ma and 46.94 +/- 0.14 Ma from the TBM provide precise constraints on the age of the fauna. These dates plus new paleomagnetic data further support the existing evidence that the TBM Fauna and the boundary between the Bridgerian and Uintan North American Land Mammal ages occurs within the lower part of Chron C21n of the Geomagnetic Polarity Time Scale. The only other fauna from North America that can confidently be assigned to biochron Ui1a is the Basal Tertiary Local Fauna from the Devil's Graveyard Formation of Texas. Revisions of the faunal characterizations of biochrons Ui1a (earliest Uintan) and Ui1b (early Uintan) of the Uintan North America Land Mammal age are proposed to further clarify their differences.
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