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
-
Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation
by: Jun Hu, et al.
Published: (2025-08-01) -
Ocean deoxygenation linked to ancient mesopelagic fish decline
by: Sven Pallacks, et al.
Published: (2025-07-01) -
Resilience of Snowball Earth to Stochastic Events
by: Guillaume Chaverot, et al.
Published: (2024-07-01) -
Microbial responses to ocean deoxygenation: Revisiting the impacts on organic carbon cycling
by: Quanrui Chen, et al.
Published: (2025-07-01) -
Characterizing the marine iodine cycle and its relationship to ocean deoxygenation in an Earth system model
by: K. Cheng, et al.
Published: (2024-11-01)