Cretaceous radiolarians of the North Atlantic Ocean

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1. Verfasser: Thurow, Juergen W
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1988
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author Thurow, Juergen W
author_facet Thurow, Juergen W
collection Datos científicos de ciencias marinas y ambientales
contents Radiolarians form a remarkable part of the fossil plankton for Cretaceous sediments of the North Atlantic. Selected sites with long-term sedimentary successions of deep facies were studied (ODP Leg 103 and DSDP Site 398 off northwest Spain and DSDP Site 603 off the east coast of the United States). Preservation of the radiolarian faunas is generally poor, and the faunal abundance and diversity reflect the diagenetic history of the host sediment rather than the original faunal productivity. Several exceptions include abundant and some well-preserved radiolarian faunas from lower Campanian, Cenomanian/Turonian boundary, upper Albian, lower Albian, and Barremian sediments. These increases in radiolarian abundance and preservation coincide with well-established Cretaceous oceanic events in the North Atlantic. Typical faunal associations of these sections are described, and faunal associations from the Cenomanian/Turonian Boundary Event are documented for the first time in the North Atlantic. The relationship of the radiolarian blooms with coeval oceanic events in the North Atlantic is also discussed.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_743398
institution PANGAEA
language en
publishDate 1988
publisher PANGAEA
record_format pangaea
spellingShingle Cretaceous radiolarians of the North Atlantic Ocean
Thurow, Juergen W
103-641A; 47-398D; 93-603B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg103; Leg47; Leg93; North Atlantic/SEAMOUNT; North Atlantic Ocean; Ocean Drilling Program; ODP
Radiolarians form a remarkable part of the fossil plankton for Cretaceous sediments of the North Atlantic. Selected sites with long-term sedimentary successions of deep facies were studied (ODP Leg 103 and DSDP Site 398 off northwest Spain and DSDP Site 603 off the east coast of the United States). Preservation of the radiolarian faunas is generally poor, and the faunal abundance and diversity reflect the diagenetic history of the host sediment rather than the original faunal productivity. Several exceptions include abundant and some well-preserved radiolarian faunas from lower Campanian, Cenomanian/Turonian boundary, upper Albian, lower Albian, and Barremian sediments. These increases in radiolarian abundance and preservation coincide with well-established Cretaceous oceanic events in the North Atlantic. Typical faunal associations of these sections are described, and faunal associations from the Cenomanian/Turonian Boundary Event are documented for the first time in the North Atlantic. The relationship of the radiolarian blooms with coeval oceanic events in the North Atlantic is also discussed.
title Cretaceous radiolarians of the North Atlantic Ocean
topic 103-641A; 47-398D; 93-603B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg103; Leg47; Leg93; North Atlantic/SEAMOUNT; North Atlantic Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.743398