Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427-Reference-Cited by-同舟云学术

Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427

Published:2022-01 Issue:1 Volume:37 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanog and Paleoclimatol

Author:

Felder Sonja¹^ORCID,Sagawa Takuya²,Greaves Mervyn³^ORCID,Leng Melanie J.⁴⁵^ORCID,Ikehara Ken⁶^ORCID,Kimoto Katsunori⁷^ORCID,Hasegawa Siro⁸,Wagner Thomas⁹^ORCID,Henderson Andrew C. G.¹^ORCID

Affiliation:

1. School of Geography, Sociology and Politics Newcastle University Newcastle Upon Tyne UK

2. Institute of Science and Engineering Kanazawa University Kanazawa Japan

3. Department of Earth Sciences University of Cambridge Cambridge UK

4. National Environmental Isotope Facility British Geological Survey Nottingham UK

5. School of Biosciences Nottingham University Nottingham UK

6. Geological Survey of Japan National Institute of Advanced Industrial Science and Technology (AIST) Tsukuba Japan

7. Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka Japan

8. The Tohoku University Museum Sendai Japan

9. The Lyell Centre School of Energy Geoscience Infrastructure and Society Heriot‐Watt University Edinburgh UK

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021PA004236

Reference160 articles.

1. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China

2. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry

3. Modelling ice sheet evolution and atmospheric CO<sub>2</sub> during the Late Pliocene

4. Modelled atmospheric temperatures and global sea levels over the past million years

5. Data report: organic matter, carbonate, and stable isotope stratigraphy from IODP Expedition 346 Sites U1426, U1427, and U1429

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