Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming-Reference-Cited by-同舟云学术

Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming

Published:2013-10 Issue:10 Volume:14 Page:4133-4152
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Baczynski Allison A.¹,McInerney Francesca A.²³,Wing Scott L.⁴,Kraus Mary J.⁵,Bloch Jonathan I.⁶,Boyer Doug M.⁷,Secord Ross⁸⁹,Morse Paul E.¹⁰,Fricke Henry C.¹¹

Affiliation:

1. Department of Earth and Planetary Sciences; Northwestern University; Technological Institute; 2145 Sheridan Road, Evanston Illinois, 60208 USA

2. Department of Earth and Planetary Sciences; Northwestern University; Evanston Illinois USA

3. Now at Sprigg Geobiology Centre; Environment Institute and School of Earth and Environmental Sciences; University of Adelaide; Adelaide, SA Australia

4. Department of Paleobiology; Smithsonian Institution; Washington D.C. USA

5. Department of Geological Sciences; University of Colorado Boulder; Boulder Colorado USA

6. Florida Museum of Natural History, University of Florida; Gainesville Florida USA

7. Department of Evolutionary Anthropology; Duke University; Durham North Carolina USA

8. Florida Museum of Natural History; University of Florida; Gainesville Florida USA

9. Now at Department of Earth and Atmospheric Sciences; University of Nebraska; Lincoln Nebraska USA

10. Florida Museum of Natural History and Department of Anthropology; University of Florida; Gainesville Florida USA

11. Department of Geology; Colorado College; Colorado Springs Colorado USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/ggge.20265/fullpdf

Reference89 articles.

1. Astronomical climate control on paleosol stacking patterns in the upper Paleocene-lower Eocene Willwood Formation, Bighorn Basin, Wyoming;Abdul Aziz;Geology,2008

2. Depletion of 13C in lignin and its implications for stable carbon isotope studies;Benner;Nature,1987

3. Terrestrial sources and export of particulate organic carbon in the Waipaoa sedimentary system: Problems, progress and processes;Blair;Mar. Geol.,2010

4. An integrated model for soil organic carbon and CO2: Implications for paleosol carbonate pCO2 paleobarometry;Bowen;Global Biogeochem. Cycles,2004

Cited by 44 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Molecular compositional variation of organic matter deposited on the East Tasman Plateau during the Paleocene–Eocene thermal maximum;SSRN Electronic Journal;2024

2. A biogeochemical perspective on pedogenesis from soils to paleosols;Reference Module in Earth Systems and Environmental Sciences;2024

3. Palynofloral Change Through the Paleocene‐Eocene Thermal Maximum in the Bighorn Basin, Wyoming;Paleoceanography and Paleoclimatology;2023-12

4. Flow depth estimates and avulsion behaviour in alluvial stratigraphy (Willwood Formation, Bighorn Basin, Wyoming, USA);The Depositional Record;2023-08-02

5. ISOORG23: An updated compilation of stable carbon isotope data of terrestrial organic materials for the Cenozoic and Mesozoic;Earth-Science Reviews;2023-06