Calcareous nannoflora response to Termination II at 45° N, 25° W (northeast Atlantic)

A. Lototskaya; P. Ziveri; G.M. Ganssen; J.E. van Hinte

doi:10.1016/S0377-8398(98)00005-X

Calcareous nannoflora response to Termination II at 45° N, 25° W (northeast Atlantic)

A. Lototskaya, P. Ziveri, G.M. Ganssen, J.E. van Hinte

Earth and Climate

Research output: Contribution to Journal › Article › Academic

Abstract

Termination II (glacial to interglacial transition from oxygen isotope stage 6 to stage 5) is considered to be one of the most rapid and abrupt climatic changes during the late Quaternary. Our high resolution geochemical and nannofloral study of the interval from 140 to 100 ka in the northeast Atlantic core T90-9P (45°17.5'N, 25°41.3'W) shows that Termination II (135-125 ka) occurred in two steps of drastic changes, interrupted by a short period of stability, and followed by at least 25 ka of relatively stable, interglacial conditions, traditionally referred to as the Eemian age (substage 5.5). A primary productivity proxy based on coccolith accumulation rate (number cm

Original language	English
Pages (from-to)	47-70
Journal	Marine Micropalaeontology
Volume	34
DOIs	https://doi.org/10.1016/S0377-8398(98)00005-X
Publication status	Published - 1998

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Lototskaya, A., Ziveri, P., Ganssen, G. M., & van Hinte, J. E. (1998). Calcareous nannoflora response to Termination II at 45° N, 25° W (northeast Atlantic). Marine Micropalaeontology, 34, 47-70. https://doi.org/10.1016/S0377-8398(98)00005-X

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abstract = "Termination II (glacial to interglacial transition from oxygen isotope stage 6 to stage 5) is considered to be one of the most rapid and abrupt climatic changes during the late Quaternary. Our high resolution geochemical and nannofloral study of the interval from 140 to 100 ka in the northeast Atlantic core T90-9P (45°17.5'N, 25°41.3'W) shows that Termination II (135-125 ka) occurred in two steps of drastic changes, interrupted by a short period of stability, and followed by at least 25 ka of relatively stable, interglacial conditions, traditionally referred to as the Eemian age (substage 5.5). A primary productivity proxy based on coccolith accumulation rate (number cm",

author = "A. Lototskaya and P. Ziveri and G.M. Ganssen and {van Hinte}, J.E.",

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T1 - Calcareous nannoflora response to Termination II at 45° N, 25° W (northeast Atlantic)

AU - Lototskaya, A.

AU - Ziveri, P.

AU - Ganssen, G.M.

AU - van Hinte, J.E.

PY - 1998

Y1 - 1998

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AB - Termination II (glacial to interglacial transition from oxygen isotope stage 6 to stage 5) is considered to be one of the most rapid and abrupt climatic changes during the late Quaternary. Our high resolution geochemical and nannofloral study of the interval from 140 to 100 ka in the northeast Atlantic core T90-9P (45°17.5'N, 25°41.3'W) shows that Termination II (135-125 ka) occurred in two steps of drastic changes, interrupted by a short period of stability, and followed by at least 25 ka of relatively stable, interglacial conditions, traditionally referred to as the Eemian age (substage 5.5). A primary productivity proxy based on coccolith accumulation rate (number cm

U2 - 10.1016/S0377-8398(98)00005-X

DO - 10.1016/S0377-8398(98)00005-X

M3 - Article

VL - 34

SP - 47

EP - 70

JO - Marine Micropalaeontology

JF - Marine Micropalaeontology

SN - 0377-8398

ER -