Nano‐Magnetite Aggregates in Red Soil on Low Magnetic Bedrock, Their Changes During Source‐Sink Transfer, and Implications for Paleoclimate Studies-Reference-Cited by-同舟云学术

Nano‐Magnetite Aggregates in Red Soil on Low Magnetic Bedrock, Their Changes During Source‐Sink Transfer, and Implications for Paleoclimate Studies

Published:2020-10 Issue:10 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Zhang Qi¹^ORCID,Appel Erwin¹^ORCID,Hu Shouyun²,Pennington Robert S.³⁴⁵,Meyer Jannik³⁴,Neumann Udo¹,Burchard Michael⁶,Allstädt Frederik⁶^ORCID,Wang Longsheng⁷,Koutsodendris Andreas⁶^ORCID

Affiliation:

1. Department of Geosciences University of Tübingen Tübingen Germany

2. Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing China

3. Institute of Applied Physics University of Tübingen Tübingen Germany

4. NMI Natural and Medical Sciences Institute University of Tübingen Reutlingen Germany

5. Department of Physics Humboldt‐Universität zu Berlin Berlin Germany

6. Institute of Earth Sciences Heidelberg University Heidelberg Germany

7. Coast Institute Ludong University Yantai China

Funder

Visiting Professorships for Senior International Scientists

Deutsche Forschungsgemeinschaft

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB020588

Reference79 articles.

1. Identification and paleoclimatic significance of magnetite nanoparticles in soils

2. Glacial-Interglacial Indian Summer Monsoon Dynamics

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4. Climate and environmental change in the Balkans over the last 17 ka recorded in sediments from Lake Prespa (Albania/F.Y.R. of Macedonia/Greece)

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