Salinity tolerance or marine organisms deduced from Red Sea Quaternary record

Amos Winter; Ahuva Almogi-Labin; Yonathan Erez; Elvira Halicz; Boaz Luz; Zeev Reiss

doi:10.1016/0025-3227(83)90030-0

Salinity tolerance or marine organisms deduced from Red Sea Quaternary record

Amos Winter, Ahuva Almogi-Labin, Yonathan Erez, Elvira Halicz, Boaz Luz, Zeev Reiss

Research output: Contribution to journal › Article › peer-review

33 Scopus citations

Abstract

The oxygen-isotopic record and microfossils from deep-sea cores raised in the hypersaline (41‰ salinity) Gulf of Aqaba indicate that during Late Quaternary glacial time salinity rose considerably due to sea-level fall and strait-dynamics, reaching values of more than 50‰ during the last Glacial maximum about 18 Ka B.P. The salinity-dependent sequence of disappearance of various species of foraminifera, pteropods and coccolithophorids can be used to determine upper salinity tolerance limits of different taxa. Only the pteropod Creseis acicula and various benthonic foraminifera are able to withstand high salinities like those during the last glacial maximum.

Original language	English
Pages (from-to)	M17-M22
Journal	Marine Geology
Volume	53
Issue number	1-2
DOIs	https://doi.org/10.1016/0025-3227(83)90030-0
State	Published - Aug 1983
Externally published	Yes

Bibliographical note

Funding Information:
Supported in part by U.S.A./Israel BSF Grant No. 1762/78 to Z. Reiss, by NSF Grant OCE 7681488 to Woods Hole Oceanographic Institution, Grant 015.7138 (to Z. Reiss) of the Israel Ministry of Energy and Intrastruc-ture and by a Lady Davis Fellowship to A. Winter.

UN SDGs

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

Access to Document

10.1016/0025-3227(83)90030-0

Cite this

@article{80e0184fd7fb4d2ea6cdda195990f597,

title = "Salinity tolerance or marine organisms deduced from Red Sea Quaternary record",

abstract = "The oxygen-isotopic record and microfossils from deep-sea cores raised in the hypersaline (41‰ salinity) Gulf of Aqaba indicate that during Late Quaternary glacial time salinity rose considerably due to sea-level fall and strait-dynamics, reaching values of more than 50‰ during the last Glacial maximum about 18 Ka B.P. The salinity-dependent sequence of disappearance of various species of foraminifera, pteropods and coccolithophorids can be used to determine upper salinity tolerance limits of different taxa. Only the pteropod Creseis acicula and various benthonic foraminifera are able to withstand high salinities like those during the last glacial maximum.",

author = "Amos Winter and Ahuva Almogi-Labin and Yonathan Erez and Elvira Halicz and Boaz Luz and Zeev Reiss",

note = "Funding Information: Supported in part by U.S.A./Israel BSF Grant No. 1762/78 to Z. Reiss, by NSF Grant OCE 7681488 to Woods Hole Oceanographic Institution, Grant 015.7138 (to Z. Reiss) of the Israel Ministry of Energy and Intrastruc-ture and by a Lady Davis Fellowship to A. Winter.",

year = "1983",

month = aug,

doi = "10.1016/0025-3227(83)90030-0",

language = "אנגלית",

volume = "53",

pages = "M17--M22",

journal = "Marine Geology",

issn = "0025-3227",

publisher = "Elsevier",

number = "1-2",

}

TY - JOUR

T1 - Salinity tolerance or marine organisms deduced from Red Sea Quaternary record

AU - Winter, Amos

AU - Almogi-Labin, Ahuva

AU - Erez, Yonathan

AU - Halicz, Elvira

AU - Luz, Boaz

AU - Reiss, Zeev

N1 - Funding Information: Supported in part by U.S.A./Israel BSF Grant No. 1762/78 to Z. Reiss, by NSF Grant OCE 7681488 to Woods Hole Oceanographic Institution, Grant 015.7138 (to Z. Reiss) of the Israel Ministry of Energy and Intrastruc-ture and by a Lady Davis Fellowship to A. Winter.

PY - 1983/8

Y1 - 1983/8

N2 - The oxygen-isotopic record and microfossils from deep-sea cores raised in the hypersaline (41‰ salinity) Gulf of Aqaba indicate that during Late Quaternary glacial time salinity rose considerably due to sea-level fall and strait-dynamics, reaching values of more than 50‰ during the last Glacial maximum about 18 Ka B.P. The salinity-dependent sequence of disappearance of various species of foraminifera, pteropods and coccolithophorids can be used to determine upper salinity tolerance limits of different taxa. Only the pteropod Creseis acicula and various benthonic foraminifera are able to withstand high salinities like those during the last glacial maximum.

AB - The oxygen-isotopic record and microfossils from deep-sea cores raised in the hypersaline (41‰ salinity) Gulf of Aqaba indicate that during Late Quaternary glacial time salinity rose considerably due to sea-level fall and strait-dynamics, reaching values of more than 50‰ during the last Glacial maximum about 18 Ka B.P. The salinity-dependent sequence of disappearance of various species of foraminifera, pteropods and coccolithophorids can be used to determine upper salinity tolerance limits of different taxa. Only the pteropod Creseis acicula and various benthonic foraminifera are able to withstand high salinities like those during the last glacial maximum.

UR - http://www.scopus.com/inward/record.url?scp=0020975223&partnerID=8YFLogxK

U2 - 10.1016/0025-3227(83)90030-0

DO - 10.1016/0025-3227(83)90030-0

M3 - ???researchoutput.researchoutputtypes.contributiontojournal.article???

AN - SCOPUS:0020975223

SN - 0025-3227

VL - 53

SP - M17-M22

JO - Marine Geology

JF - Marine Geology

IS - 1-2

ER -

Salinity tolerance or marine organisms deduced from Red Sea Quaternary record

Abstract

Bibliographical note

UN SDGs

Access to Document

Other files and links

Fingerprint

Cite this