Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Oceanic LIPs: The kiss of death

Kerr, Andrew Craig 2005. Oceanic LIPs: The kiss of death. Elements 1 (5) , pp. 289-292. 10.2113/gselements.1.5.289

Full text not available from this repository.

Abstract

Oceanic plateaus represent large areas 1 x 106 km2) of thickened oceanic crust formed from rapidly erupted lava (<3 Myr). These plateaus have formed throughout most of geological time. They generally correlate with periods of environmental catastrophe characterised by oceanic anoxia, leading to black shale formation and mass extinction events. Such correlations are particularly evident in the Cretaceous and can be partly attributed to the release of CO2 during oceanic plateau formation, which ultimately resulted in a runaway greenhouse effect. Additionally, sea level rise and disruption of oceanic circulation patterns by displacement of seawater during plateau formation contributed to increased environmental stress and biotic extinction.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Subjects: Q Science > QE Geology
Uncontrolled Keywords: Mass extinction ; Oceanic plateau ; Black shale ; Anoxia ; Mantle plume.
ISSN: 1811-5209
Last Modified: 04 Jun 2017 02:04
URI: http://orca.cf.ac.uk/id/eprint/8465

Citation Data

Cited 27 times in Google Scholar. View in Google Scholar

Actions (repository staff only)

Edit Item Edit Item