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Geochemical compositions of Neogene phosphatic brachiopods: Implications for ancient environmental and marine conditions

Geochemical compositions of Neogene phosphatic brachiopods: Implications for ancient environmental and marine conditions
Geochemical compositions of Neogene phosphatic brachiopods: Implications for ancient environmental and marine conditions
Isotopic and trace element compositions of Miocene and Pliocene phosphatic brachiopods (Lingulidae and Discinidae) from southern North Sea, the Central Paratethys and the Atlantic coast of Europe were investigated in order to trace past environmental conditions and marine connections between the northern boreal and the southern subtropical–tropical marine basins. The North Sea genus Glottidia yielded low ?Nd and high ?18OPO4 values through the Mio-Pliocene indicating cold habitat temperature where the local seawater was dominated by the Atlantic Ocean. In contrast, the Middle Miocene Lingulidae and Discinidae of the Paratethys inhabited warm subtropical seawater with the possible influence of the Indian Ocean via the Mediterranean, as supported by their average ?Nd value of ? 8.3. The combined geochemical data support a thermal and marine separation of the Paratethys from the North Sea with no direct connection or major exchange of water from the Miocene onwards.

The temperature in the Paratethys was very similar to that inferred from brachiopods from the Middle Miocene of western France, but the seawater ?Nd value here is identical to that of contemporaneous Atlantic Ocean. A Late Miocene lingulid brachiopod from southern Portugal has a high ?18OPO4, similar to the specimens investigated from the North Sea, reflecting either a deep water habitat or formation after the onset of major global cooling that resulted in an increased ?18O value of seawater. The ?Nd value of ? 8.4 for this site is compatible with an influence of Mediterranean outflow.
North Sea, Paratethys, Brachiopods, Phosphate, Isotopes, Palaeo-environment
0031-0182
66-77
Kocsis, László
a467e0c3-79db-400f-a139-8f66dffc1265
Dulai, Alfréd
89a0def7-aa5b-46b9-b2b5-1f4fe90fadb4
Bitner, Maria Aleksandra
f6785620-e9d7-4d1e-9ab8-e6d83cb73527
Vennemann, Torsten
8fa228e4-1162-4e5c-be0d-edaf8cdf8b24
Cooper, Matthew
54f7bff0-1f8c-4835-8358-71eef8529e7a
Kocsis, László
a467e0c3-79db-400f-a139-8f66dffc1265
Dulai, Alfréd
89a0def7-aa5b-46b9-b2b5-1f4fe90fadb4
Bitner, Maria Aleksandra
f6785620-e9d7-4d1e-9ab8-e6d83cb73527
Vennemann, Torsten
8fa228e4-1162-4e5c-be0d-edaf8cdf8b24
Cooper, Matthew
54f7bff0-1f8c-4835-8358-71eef8529e7a

Kocsis, László, Dulai, Alfréd, Bitner, Maria Aleksandra, Vennemann, Torsten and Cooper, Matthew (2012) Geochemical compositions of Neogene phosphatic brachiopods: Implications for ancient environmental and marine conditions. Palaeogeography Palaeoclimatology Palaeoecology, 326-328, 66-77. (doi:10.1016/j.palaeo.2012.02.004).

Record type: Article

Abstract

Isotopic and trace element compositions of Miocene and Pliocene phosphatic brachiopods (Lingulidae and Discinidae) from southern North Sea, the Central Paratethys and the Atlantic coast of Europe were investigated in order to trace past environmental conditions and marine connections between the northern boreal and the southern subtropical–tropical marine basins. The North Sea genus Glottidia yielded low ?Nd and high ?18OPO4 values through the Mio-Pliocene indicating cold habitat temperature where the local seawater was dominated by the Atlantic Ocean. In contrast, the Middle Miocene Lingulidae and Discinidae of the Paratethys inhabited warm subtropical seawater with the possible influence of the Indian Ocean via the Mediterranean, as supported by their average ?Nd value of ? 8.3. The combined geochemical data support a thermal and marine separation of the Paratethys from the North Sea with no direct connection or major exchange of water from the Miocene onwards.

The temperature in the Paratethys was very similar to that inferred from brachiopods from the Middle Miocene of western France, but the seawater ?Nd value here is identical to that of contemporaneous Atlantic Ocean. A Late Miocene lingulid brachiopod from southern Portugal has a high ?18OPO4, similar to the specimens investigated from the North Sea, reflecting either a deep water habitat or formation after the onset of major global cooling that resulted in an increased ?18O value of seawater. The ?Nd value of ? 8.4 for this site is compatible with an influence of Mediterranean outflow.

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More information

Published date: 1 April 2012
Keywords: North Sea, Paratethys, Brachiopods, Phosphate, Isotopes, Palaeo-environment
Organisations: Geochemistry

Identifiers

Local EPrints ID: 337100
URI: http://eprints.soton.ac.uk/id/eprint/337100
ISSN: 0031-0182
PURE UUID: 7103da2f-9c83-4892-98fa-a7ae9a3d6cd5
ORCID for Matthew Cooper: ORCID iD orcid.org/0000-0002-2130-2759

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Date deposited: 18 Apr 2012 09:00
Last modified: 15 Mar 2024 03:09

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Contributors

Author: László Kocsis
Author: Alfréd Dulai
Author: Maria Aleksandra Bitner
Author: Torsten Vennemann
Author: Matthew Cooper ORCID iD

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