Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...

The planktonic foraminiferal zonation of Jenkins and Srinivasan (1986), which was defined for the southwestern sector of the temperate South Pacific Ocean, was successfully extended to the temperate sequences at Site 704. The zonation is based on first and last appearances of globorotalids, principa...

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Main Author: Brunner, Charlotte A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.755426
https://doi.pangaea.de/10.1594/PANGAEA.755426
id ftdatacite:10.1594/pangaea.755426
record_format openpolar
spelling ftdatacite:10.1594/pangaea.755426 2024-09-15T18:19:31+00:00 Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ... Brunner, Charlotte A 1991 application/zip https://dx.doi.org/10.1594/pangaea.755426 https://doi.pangaea.de/10.1594/PANGAEA.755426 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.114.183.1991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg114 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1991 ftdatacite https://doi.org/10.1594/pangaea.75542610.2973/odp.proc.sr.114.183.1991 2024-08-01T10:54:44Z The planktonic foraminiferal zonation of Jenkins and Srinivasan (1986), which was defined for the southwestern sector of the temperate South Pacific Ocean, was successfully extended to the temperate sequences at Site 704. The zonation is based on first and last appearances of globorotalids, principally Globoconella species, which are indigenous to temperate surface-water masses. Most of the first and last appearances at ODP Site 704 are diachronous with those in the warmer temperate to subtropical South Atlantic, North Atlantic, and South Pacific oceans.The upper Miocene, upper Pliocene, and Quaternary sequences are punctuated by frequent incursions of subantarctic and polar assemblages of planktonic foraminifers. I assume that the appearance of an assemblage dominated by sinistral Neogloboquadrina pachyderma means that the Polar Front has migrated northward, but I do not know its position north or south of the site based on this preliminary work. The upper Miocene sequence contains five incursions between ... : Supplement to: Brunner, Charlotte A (1991): Latest Miocene to Quaternary biostratigraphy and paleoceanography, Site 704, subantarctic South Atlantic Ocean. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 201-215 ... Article in Journal/Newspaper Neogloboquadrina pachyderma North Atlantic Planktonic foraminifera South Atlantic Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
Brunner, Charlotte A
Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
topic_facet Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
description The planktonic foraminiferal zonation of Jenkins and Srinivasan (1986), which was defined for the southwestern sector of the temperate South Pacific Ocean, was successfully extended to the temperate sequences at Site 704. The zonation is based on first and last appearances of globorotalids, principally Globoconella species, which are indigenous to temperate surface-water masses. Most of the first and last appearances at ODP Site 704 are diachronous with those in the warmer temperate to subtropical South Atlantic, North Atlantic, and South Pacific oceans.The upper Miocene, upper Pliocene, and Quaternary sequences are punctuated by frequent incursions of subantarctic and polar assemblages of planktonic foraminifers. I assume that the appearance of an assemblage dominated by sinistral Neogloboquadrina pachyderma means that the Polar Front has migrated northward, but I do not know its position north or south of the site based on this preliminary work. The upper Miocene sequence contains five incursions between ... : Supplement to: Brunner, Charlotte A (1991): Latest Miocene to Quaternary biostratigraphy and paleoceanography, Site 704, subantarctic South Atlantic Ocean. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 201-215 ...
format Article in Journal/Newspaper
author Brunner, Charlotte A
author_facet Brunner, Charlotte A
author_sort Brunner, Charlotte A
title Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
title_short Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
title_full Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
title_fullStr Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
title_full_unstemmed Late Miocene to Quaternary planktonic foraminifera of ODP SIte 114-704 ...
title_sort late miocene to quaternary planktonic foraminifera of odp site 114-704 ...
publisher PANGAEA
publishDate 1991
url https://dx.doi.org/10.1594/pangaea.755426
https://doi.pangaea.de/10.1594/PANGAEA.755426
genre Neogloboquadrina pachyderma
North Atlantic
Planktonic foraminifera
South Atlantic Ocean
genre_facet Neogloboquadrina pachyderma
North Atlantic
Planktonic foraminifera
South Atlantic Ocean
op_relation https://dx.doi.org/10.2973/odp.proc.sr.114.183.1991
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.75542610.2973/odp.proc.sr.114.183.1991
_version_ 1810457865121431552