The last 1 million years of the extinct genus Discoaster: Plio-Pleistocene environment and productivity at Site U1476 (Mozambique Channel)

TitleThe last 1 million years of the extinct genus Discoaster: Plio-Pleistocene environment and productivity at Site U1476 (Mozambique Channel)
Publication TypeJournal Article
Year of Publication2018
AuthorsTangunan D.N, Baumann K.H, Just J., LeVay L.J, Barker S., Brentegani L., De Vleeschouwer D., Hall I.R, Hemming S., Norris R., Sci PExpedition
JournalPalaeogeography Palaeoclimatology Palaeoecology
Volume505
Pagination187-197
Date Published2018/09
Type of ArticleArticle
ISBN Number0031-0182
Accession NumberWOS:000438477700016
Keywords361; assemblages; atlantic; calcareous nannofossils; climate; coccolithophores; equatorial; expedition; Geology; indian-ocean; late pliocene; Nannoplankton; northern-hemisphere glaciation; oceanic primary production; Paleontology; Physical Geography; pleistocene; Western Indian Ocean
Abstract

A detailed paleoenvironment reconstruction from the Mozambique Channel, western Indian Ocean, based on the calcareous nannoplankton assemblages was conducted for the interval between 2.85 and 1.85 Myr. This study covers the period during which the successive extinction of the last five species of discoasters occurred. New productivity data obtained from the abundances of the Discoaster species (Discoaster brouweri, D. triradiatus, D. pentaradiatus, D surculus, and D. tamalis) and other indicative calcareous nannoplankton taxa showed abundance variations, which were at paced with the 100, 41, and 23 kyr astronomical periodicities. A shift in the productivity and water-column stratification proxies occurred at similar to 2.4 Ma, after the onset of the Northern Hemisphere glaciation. Here we propose that the variability recorded at International Ocean Discovery Program Site U1476 reflects the interplay between forcing associated with warm tropical Pacific and cold southern ocean influences. The former is shown by consistent occurrence of warm water taxa (Calcidiscus leptoporus, Oolithotus spp., Rhabdosphaera clavigera, Syracosphaera spp., Umbellosphaera spp.), typical of Indonesian Throughflow surface waters. On the other hand, the occurrence of Coccolithus pelagicus indicates the influence of cold, nutrient-rich sub-Antarctic surface waters. A more mixed water column initiated at similar to 2.4 Ma, and a consequent productivity increase led to the gradual reduction of the Discoaster species, until their extinction at 1.91 Ma. This period was characterized by the low values of the Florisphaera profunda index and high abundances of upper photic zone flora, indicative of nutrient-rich surface water conditions. High productivity at the location during this period could have also been amplified by localized upwelling events driven by the Mozambique Channel eddies.

DOI10.1016/j.palaeo.2018.05.043
Short TitlePaleogeogr. Paleoclimatol. Paleoecol.
Student Publication: 
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