Ocean deoxygenation after the Sturtian Snowball
Abstract The abrupt ending of the Sturtian ‘Snowball’ glaciation was characterised by enhanced chemical weathering and carbon cycle perturbations, but there is less certainty over how oxygen levels responded to those changes. Here we reconcile conflicting views using a carbonate-based multiproxy dat...
Saved in:
| Main Authors: | Kun Zhang, Susan H. Little, Alexander J. Dickson, Graham A. Shields |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-07-01
|
| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-025-60700-w |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Ocean deoxygenation linked to ancient mesopelagic fish decline
by: Sven Pallacks, et al.
Published: (2025-07-01) -
Microbial responses to ocean deoxygenation: Revisiting the impacts on organic carbon cycling
by: Quanrui Chen, et al.
Published: (2025-07-01) -
Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation
by: Jun Hu, et al.
Published: (2025-08-01) -
Biosignatures of diverse eukaryotic life from a Snowball Earth analogue environment in Antarctica
by: Fatima Husain, et al.
Published: (2025-06-01) -
Recent advances in electrochemical deoxygenative functionalization of alcohols and their derivatives
by: Yong Yuan, et al.
Published: (2025-06-01)