Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...

Significant changes in terrestrial and marine environments of Baffin Bay occurred throughout the late Pliocene to Holocene. Upper Pliocene and lowermost Pleistocene sediments contain abundant pollen and spores, which indicates the existence of open, coniferous, boreal forest to forest tundra in area...

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Main Authors: de Vernal, Anne, Mudie, Peta J
Format: Dataset
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.744818
https://doi.pangaea.de/10.1594/PANGAEA.744818
id ftdatacite:10.1594/pangaea.744818
record_format openpolar
spelling ftdatacite:10.1594/pangaea.744818 2024-09-15T17:56:54+00:00 Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ... de Vernal, Anne Mudie, Peta J 1989 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.744818 https://doi.pangaea.de/10.1594/PANGAEA.744818 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.133.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label Sample code/label 2 Dinoflagellate cyst per volume Peridiniaceae Acritarcha Pollen, total Spores Palynomorpha, terrestrial Palynomorpha, marine Pediastrum sp. Tasmanideae Drilling/drill rig DSDP/ODP/IODP sample designation Leg105 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 1989 ftdatacite https://doi.org/10.1594/pangaea.74481810.2973/odp.proc.sr.105.133.1989 2024-08-01T11:09:59Z Significant changes in terrestrial and marine environments of Baffin Bay occurred throughout the late Pliocene to Holocene. Upper Pliocene and lowermost Pleistocene sediments contain abundant pollen and spores, which indicates the existence of open, coniferous, boreal forest to forest tundra in areas surrounding Baffin Bay. The late Pliocene-earliest Pleistocene also is characterized by relatively rich, dinoflagellate cyst and acritarch assemblages of boreal character, in which the dominance of Cymatiosphaera and Peridiniaceae may indicate neritic influx of sediments. In contrast, the late-early Pleistocene to Holocene interval is marked by a sparse terrestrial and marine palynoflora, with rare productive intervals. The general paucity of the Pleistocene palynoflora suggests low primary productivity, both on land and offshore, probably caused by cold, dry, high arctic conditions. ... : Supplement to: de Vernal, Anne; Mudie, Peta J (1989): Late Pliocene to Holocene palynostratigraphy at ODP Site 645, Baffin Bay. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 387-399 ... Dataset Baffin Bay Baffin Bay Baffin Tundra DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Sample code/label
Sample code/label 2
Dinoflagellate cyst per volume
Peridiniaceae
Acritarcha
Pollen, total
Spores
Palynomorpha, terrestrial
Palynomorpha, marine
Pediastrum sp.
Tasmanideae
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Sample code/label
Sample code/label 2
Dinoflagellate cyst per volume
Peridiniaceae
Acritarcha
Pollen, total
Spores
Palynomorpha, terrestrial
Palynomorpha, marine
Pediastrum sp.
Tasmanideae
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg105
Joides Resolution
Ocean Drilling Program ODP
de Vernal, Anne
Mudie, Peta J
Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
topic_facet Sample code/label
Sample code/label 2
Dinoflagellate cyst per volume
Peridiniaceae
Acritarcha
Pollen, total
Spores
Palynomorpha, terrestrial
Palynomorpha, marine
Pediastrum sp.
Tasmanideae
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg105
Joides Resolution
Ocean Drilling Program ODP
description Significant changes in terrestrial and marine environments of Baffin Bay occurred throughout the late Pliocene to Holocene. Upper Pliocene and lowermost Pleistocene sediments contain abundant pollen and spores, which indicates the existence of open, coniferous, boreal forest to forest tundra in areas surrounding Baffin Bay. The late Pliocene-earliest Pleistocene also is characterized by relatively rich, dinoflagellate cyst and acritarch assemblages of boreal character, in which the dominance of Cymatiosphaera and Peridiniaceae may indicate neritic influx of sediments. In contrast, the late-early Pleistocene to Holocene interval is marked by a sparse terrestrial and marine palynoflora, with rare productive intervals. The general paucity of the Pleistocene palynoflora suggests low primary productivity, both on land and offshore, probably caused by cold, dry, high arctic conditions. ... : Supplement to: de Vernal, Anne; Mudie, Peta J (1989): Late Pliocene to Holocene palynostratigraphy at ODP Site 645, Baffin Bay. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 387-399 ...
format Dataset
author de Vernal, Anne
Mudie, Peta J
author_facet de Vernal, Anne
Mudie, Peta J
author_sort de Vernal, Anne
title Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
title_short Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
title_full Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
title_fullStr Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
title_full_unstemmed Palynomorph concentrations in ODP Hole 105-645B samples (Table 1) ...
title_sort palynomorph concentrations in odp hole 105-645b samples (table 1) ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.744818
https://doi.pangaea.de/10.1594/PANGAEA.744818
genre Baffin Bay
Baffin Bay
Baffin
Tundra
genre_facet Baffin Bay
Baffin Bay
Baffin
Tundra
op_relation https://dx.doi.org/10.2973/odp.proc.sr.105.133.1989
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.74481810.2973/odp.proc.sr.105.133.1989
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