Redox evolution in the subtropical Northwest Pacific across the Middle Miocene Climate Transition

2023/11/10 by Zhishun Zhang, Jun Yang, Xuguang Feng +9 · 1 voice
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.jseaes.2023.105916

openalex publication_date 2023/11/10 · crossref created 2023/11/10 · crossref issued 2024/01/01 · crossref published 2024/01/01 · crossref published-print 2024/01/01 · openalex created_date 2025/10/10 · crossref deposited 2025/10/24 · crossref indexed 2026/02/10 · openalex updated_date 2026/08/04

Citations

• Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages
• Trace metals as paleoredox and paleoproductivity proxies: An update
• Why is no deep water formed in the North Pacific?
• Drivers and mechanisms of ocean deoxygenation
• Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records
• An astronomically dated record of Earth’s climate and its predictability over the last 66 million years
• The Miocene: The Future of the Past
• Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models

Discussions

• #WeekendReading: Zhang et al., on how redox state in the north Pacific evolved in the Mid #Miocene. Definitely some interesting implications to the aging rate of Pacific waters and interbasin gradient [bsky, 0 points, 0 comments]