Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary

L. Sbaffi; F. Carlo Wezel; N. Kallel; M. Paterne; I. Cacho; P. Ziveri; N.J. Shackleton

doi:10.1016/S0025-3227(01)00185-2

Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary

L. Sbaffi
, F. Carlo Wezel
, N. Kallel
, M. Paterne
, I. Cacho
, P. Ziveri
, N.J. Shackleton

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Three central Mediterranean deep-sea cores have been studied to reconstruct the palaeoclimatic history of the basin over the time interval 34-0 kyr BP. The intensity and duration of the climatic events that occurred in the Mediterranean Sea during the last glacial-postglacial transition were estimated by observing compositional changes in the planktonic foraminifera and calcareous nannoplankton (coccolithophores) assemblages, together with a reconstruction of sea surface temperatures (using the Modern Analogue Techmque and U

Original language	English
Pages (from-to)	39-62
Journal	Marine Geology
Volume	178
DOIs	https://doi.org/10.1016/S0025-3227(01)00185-2
Publication status	Published - 2001

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 14 Life Below Water

Access to Document

10.1016/S0025-3227(01)00185-2

Persistent URL (handle)

Persistent link

Cite this

@article{cfd0e006f58542da8608f8a90eb2eb7a,

title = "Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary",

abstract = "Three central Mediterranean deep-sea cores have been studied to reconstruct the palaeoclimatic history of the basin over the time interval 34-0 kyr BP. The intensity and duration of the climatic events that occurred in the Mediterranean Sea during the last glacial-postglacial transition were estimated by observing compositional changes in the planktonic foraminifera and calcareous nannoplankton (coccolithophores) assemblages, together with a reconstruction of sea surface temperatures (using the Modern Analogue Techmque and U",

author = "L. Sbaffi and \{Carlo Wezel\}, F. and N. Kallel and M. Paterne and I. Cacho and P. Ziveri and N.J. Shackleton",

year = "2001",

doi = "10.1016/S0025-3227(01)00185-2",

language = "English",

volume = "178",

pages = "39--62",

journal = "Marine Geology",

issn = "0025-3227",

publisher = "Elsevier B.V.",

}

TY - JOUR

T1 - Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary

AU - Sbaffi, L.

AU - Carlo Wezel, F.

AU - Kallel, N.

AU - Paterne, M.

AU - Cacho, I.

AU - Ziveri, P.

AU - Shackleton, N.J.

PY - 2001

Y1 - 2001

N2 - Three central Mediterranean deep-sea cores have been studied to reconstruct the palaeoclimatic history of the basin over the time interval 34-0 kyr BP. The intensity and duration of the climatic events that occurred in the Mediterranean Sea during the last glacial-postglacial transition were estimated by observing compositional changes in the planktonic foraminifera and calcareous nannoplankton (coccolithophores) assemblages, together with a reconstruction of sea surface temperatures (using the Modern Analogue Techmque and U

AB - Three central Mediterranean deep-sea cores have been studied to reconstruct the palaeoclimatic history of the basin over the time interval 34-0 kyr BP. The intensity and duration of the climatic events that occurred in the Mediterranean Sea during the last glacial-postglacial transition were estimated by observing compositional changes in the planktonic foraminifera and calcareous nannoplankton (coccolithophores) assemblages, together with a reconstruction of sea surface temperatures (using the Modern Analogue Techmque and U

U2 - 10.1016/S0025-3227(01)00185-2

DO - 10.1016/S0025-3227(01)00185-2

M3 - Article

SN - 0025-3227

VL - 178

SP - 39

EP - 62

JO - Marine Geology

JF - Marine Geology

ER -

Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary

Abstract

UN SDGs

Access to Document

Persistent URL (handle)

Fingerprint

Cite this