Distribution of Upper Cretaceous deep water agglutinated foraminifera in sediments of the North Atlantic and its marginal seas (Tab. 1)
Citation
Kuhnt W, Kaminski M A, Moullade M (1989). Distribution of Upper Cretaceous deep water agglutinated foraminifera in sediments of the North Atlantic and its marginal seas (Tab. 1). PANGAEA - Data Publisher for Earth & Environmental Science. Occurrence dataset https://doi.org/10.1594/pangaea.667860 accessed via GBIF.org on 2024-08-17.Description
The stratigraphic and biogeographic distribution of more than 170 species of deep-water agglutinated benthic foraminifers (DWAF) from the North Atlantic and adjacent marginal seas has been compared with paleoenvironmental data (e.g. paleobathymetry, oxygenation of the bottom waters, amount of terrigenous input and substrate disturbance). Six general types of assemblages, in which deep water agglutinated taxa occur, are defined from the Turonian to Maastrichtian times: 1. High latitude slope assemblages 2. Low to mid latitude slope assemblages 3. Flysch-type assemblages 4. Deep water limestone assemblages (,,Scaglia,,-type) 5. Abyssal mixed calcareous-agglutinated assemblages 6. Abyssal purely agglutinated assemblages Latitudinal differences in faunal composition are observed, the most important of which is the lack or extreme paucity of calcareous forms in high latitude assemblages. East-to-west differences appear to be of comparatively minor importance. Most DWAF species occur in all studied regions and are thus considered as cosmopolitan. Biostratigraphic turnovers in the taxonomic content of assemblages are observed in the lowermost Turonian, mid-Campanian and in the upper Maastrichtian to lowermost Paleocene. These datum levels correspond to inter-regional and time-constant paleooceanographic events, which probably also affected the deep-water benthic biota. This allows us to use deep-water agglutinated foraminifers for biostratigraphy in the North Atlantic sequences deposited below CCD and to geographically extend the currently used zonal schemes which have been established in the Carpathian and Alpine areas.Taxonomic Coverages
-
Chromistarank: kingdom
-
Foraminiferarank: kingdom
Geographic Coverages
Event: 14-137,
North Atlantic/HILL
; Event: 14-141,
North Atlantic/DIAPIR
; Event: 41-367,
North Atlantic/BASIN
; Event: 41-368,
North Atlantic/CONT RISE
; Event: 78-543A,
North Atlantic/CONT RISE
; Event: 93-603B, ; Event: 103-641A,
South Atlantic Ocean
; Event: Gibralta_arch,
Spain
; Event: Gubbio,
Italy
; Event: Indian_Habour,
Labrador
; Event: Mesoriff_zone,
Moroccan margin
; Event: Penibetic_zone,
Spain
; Event: Trinidad, ; Event: Zumaya_section,
Spain
;
Bibliographic Citations
Contacts
Wolfgang Kuhntoriginator
Michael Anthony Kaminski
originator
Michel Moullade
originator
metadata author
PANGAEA - Data Publisher for Earth & Environmental Science
email: info@pangaea.de
homepage: https://www.pangaea.de
Frank-Oliver Glöckner
administrative point of contact
Robert Huber
administrative point of contact