Age model tie points of ODP Sites in the central Atlantic Ocean

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Auteurs principaux: Gibbs, Samantha J, Young, Jeremy, Bralower, Timothy J, Shackleton, Nicholas J
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2005
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_version_ 1867171356638969856
author Gibbs, Samantha J
Young, Jeremy
Bralower, Timothy J
Shackleton, Nicholas J
author_facet Gibbs, Samantha J
Young, Jeremy
Bralower, Timothy J
Shackleton, Nicholas J
collection Datos científicos de ciencias marinas y ambientales
contents The mid-Pliocene was an interval of subtle reorganisation within the nannoplankton community, including the prominent and biostratigraphically important last occurrences of Sphenolithus abies and Reticulofenestra pseudoumbilicus. The transition is part of the Pliocene to Recent "attrition" of nannofossil species that resulted from changes in the distribution of trophic resources, and deep-water and surface-water current systems, likely associated with the initiation of Northern Hemisphere glaciation. The extinctions of Sphenolithus abies and Reticulofenestra pseudoumbilicus were analysed in detail at ODP Sites 659, 662, and 926 in the equatorial and subequatorial Atlantic. These taxa show significantly different patterns of duration and timing of decline based on high-resolution abundance records and calibration with oxygen isotope stratigraphy. The initiation of abundance decline between 3.71 and 3.67 Ma and the extinction of S. abies between 3.56 and 3.52 Ma are diachronous. This extinction may have been a response to the intensification of glacial intervals at this time. In contrast, the last occurrence of R. pseudoumbilicus at 3.81-3.82 Ma appears to be a valid example of biostratigraphic (although not necessarily biological) synchrony in the fossil record. Direct environmental forcing is not attributable for the extinction of R. pseudoumbilicus; however, indirect physical and/or biological environmental stress may explain the observed patterns.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_694086
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle Age model tie points of ODP Sites in the central Atlantic Ocean
Gibbs, Samantha J
Young, Jeremy
Bralower, Timothy J
Shackleton, Nicholas J
108-659; 108-662A; 154-926A; 154-926C; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg108; Leg154; North Atlantic Ocean; Ocean Drilling Program; ODP; South Atlantic Ocean
The mid-Pliocene was an interval of subtle reorganisation within the nannoplankton community, including the prominent and biostratigraphically important last occurrences of Sphenolithus abies and Reticulofenestra pseudoumbilicus. The transition is part of the Pliocene to Recent "attrition" of nannofossil species that resulted from changes in the distribution of trophic resources, and deep-water and surface-water current systems, likely associated with the initiation of Northern Hemisphere glaciation. The extinctions of Sphenolithus abies and Reticulofenestra pseudoumbilicus were analysed in detail at ODP Sites 659, 662, and 926 in the equatorial and subequatorial Atlantic. These taxa show significantly different patterns of duration and timing of decline based on high-resolution abundance records and calibration with oxygen isotope stratigraphy. The initiation of abundance decline between 3.71 and 3.67 Ma and the extinction of S. abies between 3.56 and 3.52 Ma are diachronous. This extinction may have been a response to the intensification of glacial intervals at this time. In contrast, the last occurrence of R. pseudoumbilicus at 3.81-3.82 Ma appears to be a valid example of biostratigraphic (although not necessarily biological) synchrony in the fossil record. Direct environmental forcing is not attributable for the extinction of R. pseudoumbilicus; however, indirect physical and/or biological environmental stress may explain the observed patterns.
title Age model tie points of ODP Sites in the central Atlantic Ocean
topic 108-659; 108-662A; 154-926A; 154-926C; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg108; Leg154; North Atlantic Ocean; Ocean Drilling Program; ODP; South Atlantic Ocean
url https://doi.org/10.1594/PANGAEA.694086