Ice core evidence for atmospheric oxygen decline since the Mid-Pleistocene transition-Reference-Cited by-同舟云学术

Ice core evidence for atmospheric oxygen decline since the Mid-Pleistocene transition

Author:

Yan Yuzhen¹²^ORCID,Brook Edward J.³^ORCID,Kurbatov Andrei V.⁴^ORCID,Severinghaus Jeffrey P.⁵^ORCID,Higgins John A.¹

Affiliation:

1. Department of Geosciences, Princeton University, Princeton, NJ, USA.

2. Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX, USA.

3. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA.

4. Climate Change Institute, University of Maine, Orono, ME, USA.

5. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA.

Abstract

The 1.5-million-year-old Antarctic ice indicates a balanced atmospheric oxygen budget before the Mid-Pleistocene Transition.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference79 articles.

Cited by 8 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

2. Blue ice core sites;Reference Module in Earth Systems and Environmental Sciences;2024