Hydrologic Changes Drove the Late Miocene Expansion of C 4 Grasslands on the Northern Indian Subcontinent-Reference-Cited by-同舟云学术

Hydrologic Changes Drove the Late Miocene Expansion of C 4 Grasslands on the Northern Indian Subcontinent

Published:2021-04 Issue:4 Volume:36 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanogr Paleoclimatol

Author:

Polissar Pratigya J.¹^ORCID,Uno Kevin T.²^ORCID,Phelps Samuel R.²³^ORCID,Karp Allison T.⁴⁵^ORCID,Freeman Katherine H.⁴^ORCID,Pensky Jennifer L.⁶⁷^ORCID

Affiliation:

1. Department of Ocean Sciences University of California, Santa Cruz Santa Cruz CA USA

2. Division of Biology and Paleo Environment Lamont‐Doherty Earth Observatory of Columbia University Palisades NY USA

3. Now at Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

4. Department of Geosciences The Pennsylvania State University University Park PA USA

5. Now at Department of Ecology and Evolution Yale University New Haven CT USA

6. Barnard College New York NY USA

7. Now at Department of Earth and Planetary Science University of California Santa Cruz Santa Cruz CA USA

Funder

National Science Foundation

Lamont-Doherty Earth Observatory, Columbia University

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020PA004108

Reference148 articles.

1. Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon

2. Assessment of n-alkanes, long-chain fatty alcohols and long-chain fatty acids as diet composition markers: The concentrations of these compounds in rangeland species from Sudan

3. Evolution and origin of the Central Grassland of North America: climate, fire, and mammalian grazers1

4. Initial Expansion of C 4 Vegetation in Australia During the Late Pliocene

5. Molecular distribution and carbon isotope of n -alkanes from Ashtamudi Estuary, South India: Assessment of organic matter sources and paleoclimatic implications

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