Radiolarian abundance of sediment core Y8 ...

A high-resolution record of radiolarian faunal changes from Site Y8 south of the Subtropical Front (STF), offshore eastern New Zealand, provides insight into the paleoceanographic history of the last 265 kyrs. Quantitative analysis of radiolarian paleotemperature indicators and radiolarian-based sea...

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Bibliographic Details
Main Authors: Lüer, Vanessa, Cortese, Giuseppe, Neil, Helen L, Hollis, Christopher J, Willems, Helmut
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.691487
https://doi.pangaea.de/10.1594/PANGAEA.691487
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Summary:A high-resolution record of radiolarian faunal changes from Site Y8 south of the Subtropical Front (STF), offshore eastern New Zealand, provides insight into the paleoceanographic history of the last 265 kyrs. Quantitative analysis of radiolarian paleotemperature indicators and radiolarian-based sea surface temperature (SST) estimates reveal distinct shifts during glacial-interglacial (G-I) climate cycles encompassing marine isotope stages (MIS) 8-1. Faunas at Site Y8 are abundant and diverse and consist of a mixture of species typical of the subantarctic, transitional and subtropical zones which is characteristic of subantarctic waters just south of the STF. During interglacials, diverse radiolarian faunas have increased numbers of warm-water taxa (not, vert, similar 15%) while cool-water taxa decrease to not, vert, similar 11% of the assemblage. Warmest climate conditions occurred during MIS 5.5 and the early Holocene Climatic Optimum (HCO) at the onset of MIS 1 where SSTs reach maxima of 12.8 and 12.9 °C, ... : Supplement to: Lüer, Vanessa; Cortese, Giuseppe; Neil, Helen L; Hollis, Christopher J; Willems, Helmut (2009): Radiolarian-based sea surface temperatures and paleoceanographic changes during the Late Pleistocene-Holocene in the subantarctic southwest Pacific. Marine Micropaleontology, 70(3-4), 151-165 ...