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  4. Deciphering the palaeoecology of Late Pliocene and Early Pleistocene dinoflagellate cysts
 
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Deciphering the palaeoecology of Late Pliocene and Early Pleistocene dinoflagellate cysts

Journal
Palaeogeography, Palaeoclimatology, Palaeoecology
Journal Volume
309
Journal Issue
44563
Pages
17-32
Date Issued
2011
Author(s)
De Schepper S
Fischer E.I
JEROEN GROENEVELD  
Head M.J
Matthiessen J.
DOI
10.1016/j.palaeo.2011.04.020
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-79960644196&doi=10.1016%2fj.palaeo.2011.04.020&partnerID=40&md5=10af83cac7816ef0131f0f7791e308fb
https://scholars.lib.ntu.edu.tw/handle/123456789/624791
Abstract
In an attempt to document the palaeoecological affinities of individual extant and extinct dinoflagellate cysts, Late Pliocene and Early Pleistocene dinoflagellate cyst assemblages have been compared with geochemical data from the same samples. Mg/Ca ratios of Globigerina bulloides were measured to estimate the spring-summer sea-surface temperatures from four North Atlantic IODP/DSDP sites. Currently, our Pliocene-Pleistocene database contains 204 dinoflagellate cyst samples calibrated to geochemical data. This palaeo-database is compared with modern North Atlantic and global datasets. The focus lies in the quantitative relationship between Mg/Ca-based (i.e. spring-summer) sea-surface temperatures (SSTMg/Ca) and dinoflagellate cyst distributions. In general, extant species are shown to have comparable spring-summer SST ranges in the past (SSTMg/Ca) and today (SST from World Ocean Atlas 2005, Locarnini et al., 2006), demonstrating that our new approach is valid for inferring spring-summer SST ranges for extinct species. For example, Habibacysta tectata represents SSTMg/Ca values between 10 and 15°C when it exceeds 30% of the assemblage, and Invertocysta lacrymosa exceeds 15% when SSTMg/Ca values are between 18.6 and 23.5°C. However, comparing Pliocene and Pleistocene SSTMg/Ca values with present day summer values for the extant Impagidinium pallidum suggests a greater tolerance of higher temperatures in the past. This species occupies more than 5% of the assemblage at SSTMg/Ca values of 11.6-17.9°C in the Pliocene and Pleistocene, whereas present day summer SSTs are around - 1.7 to 6.9°C. This observation questions the value of Impagidinium pallidum as reliable indicator of cold waters in older deposits, and may explain its bipolar distribution. © 2011 Elsevier B.V.
Subjects
Dinocyst; Mg/Ca geochemistry; North Atlantic; Palaeoecology; Quaternary; Transfer function
SDGs

[SDGs]SDG14

Other Subjects
calcium; data set; database; Deep Sea Drilling Project; dinoflagellate cyst; geochemistry; high temperature; magnesium; micropaleontology; paleoecology; paleotemperature; Pleistocene; Pliocene; sea surface temperature; temperature tolerance; transfer function; Atlantic Ocean; Atlantic Ocean (North); Dinophyceae; Globigerina bulloides; Impagidinium
Type
journal article

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