CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS
Pelagic Cretaceous sediments, deposited in a range of palaeotectonic and palaeogeographic settings, from continents to oceans, are commonly black and bituminous. 3 particular time-envelopes define the major occurrences of such facies. These intervals define the duration of so-called Oceanic Anoxic E...
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Format: | Journal article |
Language: | English |
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1980
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author | Jenkyns, H |
author_facet | Jenkyns, H |
author_sort | Jenkyns, H |
collection | OXFORD |
description | Pelagic Cretaceous sediments, deposited in a range of palaeotectonic and palaeogeographic settings, from continents to oceans, are commonly black and bituminous. 3 particular time-envelopes define the major occurrences of such facies. These intervals define the duration of so-called Oceanic Anoxic Events during which global marine waters were relatively depleted in oxygen, and deposition of organic matter, derived from both terrestrial and planktonic sources, was widespread. Cretaceous OAEs correlate closely with transgressions, and such a correlation exists throughout the stratigraphical column. -from Author |
first_indexed | 2024-03-07T04:04:23Z |
format | Journal article |
id | oxford-uuid:c5a6d48d-78a2-4a71-8a09-7815489ea43e |
institution | University of Oxford |
language | English |
last_indexed | 2024-03-07T04:04:23Z |
publishDate | 1980 |
record_format | dspace |
spelling | oxford-uuid:c5a6d48d-78a2-4a71-8a09-7815489ea43e2022-03-27T06:32:34ZCRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANSJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:c5a6d48d-78a2-4a71-8a09-7815489ea43eEnglishSymplectic Elements at Oxford1980Jenkyns, HPelagic Cretaceous sediments, deposited in a range of palaeotectonic and palaeogeographic settings, from continents to oceans, are commonly black and bituminous. 3 particular time-envelopes define the major occurrences of such facies. These intervals define the duration of so-called Oceanic Anoxic Events during which global marine waters were relatively depleted in oxygen, and deposition of organic matter, derived from both terrestrial and planktonic sources, was widespread. Cretaceous OAEs correlate closely with transgressions, and such a correlation exists throughout the stratigraphical column. -from Author |
spellingShingle | Jenkyns, H CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title | CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title_full | CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title_fullStr | CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title_full_unstemmed | CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title_short | CRETACEOUS ANOXIC EVENTS - FROM CONTINENTS TO OCEANS |
title_sort | cretaceous anoxic events from continents to oceans |
work_keys_str_mv | AT jenkynsh cretaceousanoxiceventsfromcontinentstooceans |