The Paleocene−Eocene Thermal Maximum (PETM) was a brief yet extreme warming event that profoundly affected marine ecosystems, whereas its impact on contemporaneous lacustrine systems remains less well constrained. This event highlights the fundamentally different responses of marine and terrestrial ecosystems to rapid...
Cheng Wu, Lin Chen, Thomas J. Algeo et al.· Geological Society of Americ...· 0 citations
Deep-time hyperthermal/transient warming events provide critical analogs for modern climatic warming and its impacts. However, all ancient hyperthermals documented to date have occurred under greenhouse climate states, limiting their relevance for understanding the trajectory of present-day climate change. Here, we pre...
L. Yao, Thomas J. Algeo, Qiu-Lai Wang et al.· Proceedings of the National...· 0 citations
The Ediacaran Period (635–539 Ma) witnessed the emergence of early animals, rapid oceanic oxygenation, and rising oceanic P availability. However, the relationships among these developments remain intensely debated. Here, we present high-resolution carbonate-associated phosphate (CAP) data from seven Ediacaran sections...
Matthew S. Dodd, Chao Li, Meng Cheng et al.· Nature Communications· 0 citations
The pattern and cause of upper‐water temperature (UWT) variations on millennial timescales in the Southern Ocean (SO) and the mechanism of their interaction with high‐latitude Northern Hemisphere climate remain unclear. Here, we reconstructed millennial‐scale subsurface temperature (subST) records from the Weddell Sea...
Tong Wang, Thomas J. Algeo, Qi Jia et al.· Geophysical Research Letters· 0 citations
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