A Depth‐Transect of Ocean Deoxygenation During the Paleocene‐Eocene Thermal Maximum: Magnetofossils in Sediment Cores From the Southeast Atlantic-Reference-Cited by-同舟云学术

A Depth‐Transect of Ocean Deoxygenation During the Paleocene‐Eocene Thermal Maximum: Magnetofossils in Sediment Cores From the Southeast Atlantic

Author:

Xue Pengfei¹,Chang Liao¹²^ORCID,Dickens Gerald R.³^ORCID,Thomas Ellen⁴⁵^ORCID

Affiliation:

1. Laboratory of Orogenic Belts and Crustal Evolution School of Earth and Space Sciences Peking University Beijing China

2. Laboratory for Marine Geology Qingdao National Laboratory for Marine Science and Technology Qingdao China

3. Department of Geology Trinity College Dublin Dublin Ireland

4. Department of Earth and Planetary Sciences Yale University New Haven CT USA

5. Department of Earth and Environmental Sciences Wesleyan University Middletown CT USA

Funder

National Natural Science Foundation of China

Royal Society

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference95 articles.

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