Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a)
Large igneous province (LIP) volcanism has been proposed as a key trigger of several major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale carbon emissions associated with one or both of magmatic degassing from the Greater Ontong Java Plateau (G-OJP) and intrusion of...
Autors principals: | Percival, LME, Tedeschi, LR, Creaser, RA, Mather, TA, Jenkyns, HC, Et al. |
---|---|
Format: | Journal article |
Idioma: | English |
Publicat: |
Elsevier
2021
|
Ítems similars
-
Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian)
per: Jenkyns, H
Publicat: (2018) -
Phosphorus and trace-metal records during Cretaceous oceanic anoxic events: Example of the Early Aptian OAE in the western Tethys
per: Westermann Stéphane, et al.
Publicat: (2007-05-01) -
Osmium-isotope evidence for volcanism, weathering, and ocean mixing during the early Aptian OAE 1a
per: Bottini, C, et al.
Publicat: (2012) -
Aptian carbon-isotope record from the Sergipe-Alagoas Basin: New insights into oceanic anoxic event 1a and the timing of seawater entry into the South Atlantic
per: Tedeschi, LR, et al.
Publicat: (2019) -
Integrated cyclostratigraphy of the Cau core (SE Spain) - a timescale for climate change during the early Aptian Anoxic Event (OAE 1a) and the late Aptian
per: Martínez-Rodríguez, R, et al.
Publicat: (2024)