Isotopic stages of DSDP Site 94-607 (Table 1) ...

High resolution palynological analysis of DSDP Cores 607/607A shows for the interval between 2.8 and 2.2 Ma B.P. (which includes the onset of major northern hemisphere glaciations) a 41 ka cyclicity characterised by much higher palynomorph concentrations for the cooler intervals than for the warmer...

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Main Authors: Versteegh, Gerard J M, Brinkhuis, Henk, Visscher, Henk, Zonneveld, Karin A F
Format: Dataset
Language:English
Published: PANGAEA 1996
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.742722
https://doi.pangaea.de/10.1594/PANGAEA.742722
id ftdatacite:10.1594/pangaea.742722
record_format openpolar
spelling ftdatacite:10.1594/pangaea.742722 2024-09-15T18:23:34+00:00 Isotopic stages of DSDP Site 94-607 (Table 1) ... Versteegh, Gerard J M Brinkhuis, Henk Visscher, Henk Zonneveld, Karin A F 1996 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.742722 https://doi.pangaea.de/10.1594/PANGAEA.742722 en eng PANGAEA https://dx.doi.org/10.1016/0921-8181(95)00054-2 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Isotopic event DEPTH, sediment/rock Age model Composite Core Age model calibration Leg94 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1996 ftdatacite https://doi.org/10.1594/pangaea.74272210.1016/0921-8181(95)00054-2 2024-08-01T10:58:30Z High resolution palynological analysis of DSDP Cores 607/607A shows for the interval between 2.8 and 2.2 Ma B.P. (which includes the onset of major northern hemisphere glaciations) a 41 ka cyclicity characterised by much higher palynomorph concentrations for the cooler intervals than for the warmer ones. Variation in dilution and concentration of palynomorphs can neither be explained by differential input of terrigenous clastics or carbonate, nor by differences in sedimentation rate, sediment density or selective preservation of palynomorphs. Subdivision of the palynomorph record in terms of autochthonous and allochthonous components, provides a way to detect changes in open ocean productivity and transport through time. It seems that a negative correlation between productivity and temperature in the latest Pleistocene open Atlantic had already been established before the major onset of northern hemisphere glaciations. A conceptual model is proposed to explain the observed lead of the palynological record ... : Supplement to: Versteegh, Gerard J M; Brinkhuis, Henk; Visscher, Henk; Zonneveld, Karin A F (1996): The relation between productivity and temperature in the Pliocene North Atlantic at the onset of northern hemisphere glaciation: a palynological study. Global and Planetary Change, 11(4), 155165 ... Dataset North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Isotopic event
DEPTH, sediment/rock
Age model
Composite Core
Age model calibration
Leg94
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Isotopic event
DEPTH, sediment/rock
Age model
Composite Core
Age model calibration
Leg94
Glomar Challenger
Deep Sea Drilling Project DSDP
Versteegh, Gerard J M
Brinkhuis, Henk
Visscher, Henk
Zonneveld, Karin A F
Isotopic stages of DSDP Site 94-607 (Table 1) ...
topic_facet Isotopic event
DEPTH, sediment/rock
Age model
Composite Core
Age model calibration
Leg94
Glomar Challenger
Deep Sea Drilling Project DSDP
description High resolution palynological analysis of DSDP Cores 607/607A shows for the interval between 2.8 and 2.2 Ma B.P. (which includes the onset of major northern hemisphere glaciations) a 41 ka cyclicity characterised by much higher palynomorph concentrations for the cooler intervals than for the warmer ones. Variation in dilution and concentration of palynomorphs can neither be explained by differential input of terrigenous clastics or carbonate, nor by differences in sedimentation rate, sediment density or selective preservation of palynomorphs. Subdivision of the palynomorph record in terms of autochthonous and allochthonous components, provides a way to detect changes in open ocean productivity and transport through time. It seems that a negative correlation between productivity and temperature in the latest Pleistocene open Atlantic had already been established before the major onset of northern hemisphere glaciations. A conceptual model is proposed to explain the observed lead of the palynological record ... : Supplement to: Versteegh, Gerard J M; Brinkhuis, Henk; Visscher, Henk; Zonneveld, Karin A F (1996): The relation between productivity and temperature in the Pliocene North Atlantic at the onset of northern hemisphere glaciation: a palynological study. Global and Planetary Change, 11(4), 155165 ...
format Dataset
author Versteegh, Gerard J M
Brinkhuis, Henk
Visscher, Henk
Zonneveld, Karin A F
author_facet Versteegh, Gerard J M
Brinkhuis, Henk
Visscher, Henk
Zonneveld, Karin A F
author_sort Versteegh, Gerard J M
title Isotopic stages of DSDP Site 94-607 (Table 1) ...
title_short Isotopic stages of DSDP Site 94-607 (Table 1) ...
title_full Isotopic stages of DSDP Site 94-607 (Table 1) ...
title_fullStr Isotopic stages of DSDP Site 94-607 (Table 1) ...
title_full_unstemmed Isotopic stages of DSDP Site 94-607 (Table 1) ...
title_sort isotopic stages of dsdp site 94-607 (table 1) ...
publisher PANGAEA
publishDate 1996
url https://dx.doi.org/10.1594/pangaea.742722
https://doi.pangaea.de/10.1594/PANGAEA.742722
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1016/0921-8181(95)00054-2
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.74272210.1016/0921-8181(95)00054-2
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