Widespread upper-ocean deoxygenation in the Alpine-Mediterranean Tethys during the Toarcian Oceanic Anoxic Event
The early Toarcian (∼183 Ma) was characterized by pronounced climate warming associated with massive release of 13C-depleted carbon to the exogenic system, as evidenced by globally recognized negative carbon-isotope excursions (N-CIE) in biospheric carbon reservoirs. Global warming during this inter...
| Những tác giả chính: | Chen, W, Kemp, DB, Jenkyns, HC, Robinson, SA, Jiang, S, Pan, C, Li, C |
|---|---|
| Định dạng: | Journal article |
| Ngôn ngữ: | English |
| Được phát hành: |
Elsevier
2024
|
Những quyển sách tương tự
-
An open ocean record of the Toarcian oceanic anoxic event
Bằng: D. R. Gröcke, et al.
Được phát hành: (2011-11-01) -
Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
Bằng: E. Erba, et al.
Được phát hành: (2019-12-01) -
The Toarcian Oceanic Anoxic Event in the Ionian Zone, Greece
Bằng: Kafousia, N, et al.
Được phát hành: (2014) -
A global perturbation to the sulfur cycle during the Toarcian Oceanic Anoxic Event
Bằng: Gill, B, et al.
Được phát hành: (2011) -
Molybdenum-isotope chemostratigraphy and paleoceanography of the Toarcian Oceanic Anoxic Event (Early Jurassic)
Bằng: Dickson, A, et al.
Được phát hành: (2017)