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  4. Dinoflagellate cyst paleoecology during the Pliocene–Pleistocene climatic transition in the North Atlantic
 
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Dinoflagellate cyst paleoecology during the Pliocene–Pleistocene climatic transition in the North Atlantic

Journal
Palaeogeography, Palaeoclimatology, Palaeoecology
Journal Volume
470
Pages
81-108
Date Issued
2017
Author(s)
Hennissen J.A.I
Head M.J
De Schepper S
JEROEN GROENEVELD  
DOI
10.1016/j.palaeo.2016.12.023
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85009910026&doi=10.1016%2fj.palaeo.2016.12.023&partnerID=40&md5=06929f91bb5e2e34313ba596c3ea408d
https://scholars.lib.ntu.edu.tw/handle/123456789/624759
Abstract
Dinoflagellate cysts (dinocysts) are widely used as tracers of sea surface conditions in late Quaternary marine records. However, paleoenvironmental reconstructions across the Pliocene–Pleistocene climatic transition and beyond are limited because the hydrologic conditions influencing assemblage compositions may not have a modern analogue, and the ecological optima of extinct dinocyst species are not well known. From a study of two cored sites in the central and eastern North Atlantic, we bypass these issues by statistically analyzing the variations in dinocyst assemblage composition and comparing the results directly to paleoecological parameters (δ18Obulloides, δ18Osalinity, and geochemical proxies for sea surface temperature [SST]) derived from the planktonic foraminifer Globigerina bulloides recovered from the same samples as the dinocysts. Through canonical correspondence analysis we demonstrate the co-variation of seasonality and dinocyst paleoproductivity. We show that Pyxidinopsis braboi is a cold tolerant species with an optimum SST between 12 and 14 °C. We extend the use of Nematosphaeropsis labyrinthus as an indicator of transitional climatic conditions to the Pliocene, we offer evidence for the correlation of Bitectatodinium tepikiense and Filisphaera microornata to high seasonality, and we reiterate an apparent link between Spiniferites mirabilis and eastern North Atlantic water masses. Finally, we confirm that Habibacysta tectata is cold-tolerant rather than a strictly cold-water indicator, that Operculodinium? eirikianum is a cold-intolerant species favoring outer neritic environments, and that Ataxiodinium confusum and Invertocysta lacrymosa are both warm-water species. © 2017 Elsevier B.V.
SDGs

[SDGs]SDG14

Other Subjects
bioindicator; climate variation; cold tolerance; core analysis; dinoflagellate cyst; geochemical survey; hydrological regime; paleoecology; paleoproductivity; Pliocene-Pleistocene boundary; sea surface temperature; water mass; Atlantic Ocean; Atlantic Ocean (North); Bitectatodinium tepikiense; Dinophyceae; Foraminifera; Globigerina bulloides; Nematosphaeropsis labyrinthus; Operculodinium; Pyxidinopsis braboi; Spiniferites mirabilis
Type
journal article

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