Identifying Hydro‐Sensitive Coral δ <sup>18</sup> O Records for Improved High‐Resolution Temperature and Salinity Reconstructions-Reference-Cited by-同舟云学术

Identifying Hydro‐Sensitive Coral δ ¹⁸ O Records for Improved High‐Resolution Temperature and Salinity Reconstructions

Published:2022-05-07 Issue:9 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Thompson D. M.¹^ORCID,Conroy J. L.²^ORCID,Konecky B. L.³^ORCID,Stevenson S.⁴^ORCID,DeLong K. L.⁵^ORCID,McKay N.⁶^ORCID,Reed E.¹^ORCID,Jonkers L.⁷^ORCID,Carré M.⁸^ORCID

Affiliation:

1. Department of Geosciences University of Arizona Tucson AZ USA

2. Department of Geology and Department of Plant Biology University of Illinois Urbana‐Champaign IL USA

3. Department of Earth and Planetary Sciences Washington University Saint Louis MO USA

4. Bren School of Environmental Science & Management University of California Santa Barbara CA USA

5. Department of Geography and Anthropology Coastal Studies Institute Louisiana State University Baton Rouge LA USA

6. School of Earth and Sustainability Northern Arizona University Flagstaff AZ USA

7. MARUM Center for Marine Environmental Sciences Bremen University Bremen Germany

8. IPSL‐LOCEAN Laboratory Sorbonne Universités (UPMC)‐CNRS‐IRD‐MNHN Paris France

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL096153

Reference113 articles.

1. Oxygen isotopes, upper-ocean salinity, and precipitation sources in the eastern tropical Pacific

2. Twentieth century sea surface temperature and salinity variations at Timor inferred from paired coral δ18O and Sr/Ca measurements

3. Reconstructing seawater δ18O from paired coral δ18O and Sr/Ca ratios: Methods, error analysis and problems, with examples from Tahiti (French Polynesia) and Timor (Indonesia)

4. High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene

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