In:
AGU Advances, American Geophysical Union (AGU), Vol. 1, No. 4 ( 2020-12)
Abstract:
Sediments derived from decarbonation of the Chicxulub impact target were deposited by tsunami and seiche waves over months to years followed by a layer with atmospheric fallout Temperatures in the ocean above the hotter regions of the crater were in excess of 70°C, with heat likely derived from the central impact melt pool Cooler regions within the crater basin became habitats soon after impact with diverse life ranging from microbes to marine arthropods, and possibly fish
Type of Medium:
Online Resource
ISSN:
2576-604X
,
2576-604X
DOI:
10.1029/2020AV000208
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
3008306-0
