(Q58394254)

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Holocene Climate Optimum and Last Glacial Maximum in the Mediterranean: the marine oxygen isotope record

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title

Holocene Climate Optimum and Last Glacial Maximum in the Mediterranean: the marine oxygen isotope record (English)

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1

Eelco J. Rohling

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author name string

S. De Rijk

series ordinal

2

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publication date

January 1999

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published in

Marine Geology

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volume

153

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issue

1-4

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page(s)

57-75

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cites work

Reef drowning during the last deglaciation: Evidence for catastrophic sea-level rise and ice-sheet collapse

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7 January 2021

Tellus A: Dynamic Meteorology and Oceanography, Volume 73, Issue 1 (2021)

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7 January 2021

Variation of O18 content of waters from natural sources

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7 January 2021

A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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7 January 2021

Late Quaternary central Mediterranean biochronology

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7 January 2021

Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years

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7 January 2021

Postglacial connection of the Black Sea to the Mediterranean and its relation to the timing of sapropel formation

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Surface water temperature, salinity, and density changes in the northeast Atlantic during the last 45,000 years: Heinrich events, deep water formation, and climatic rebounds

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7 January 2021

Oxygen Isotope Fractionation in Divalent Metal Carbonates

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7 January 2021

A Simple Two-Layered Model for Shoaling of the Eastern Mediterranean Pycnocline Due to Glacio-Eustatic Sea Level Lowering

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7 January 2021

Review and new aspects concerning the formation of eastern Mediterranean sapropels

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Northern Levantine and Adriatic Quaternary planktic foraminifera; Reconstruction of paleoenvironmental gradients

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7 January 2021

200 Year interruption of Holocene sapropel formation in the Adriatic Sea

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7 January 2021

After the deluge: Mediterranean stagnation and sapropel formation

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7 January 2021

Glacial–Holocene salinity changes in the Mediterranean Sea: hydrographic and depositional effects

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7 January 2021

The age and origin of the “Younger Dryas climate event” in Greenland ice cores

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7 January 2021

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Palaeoceanography of the last deglaciation in the Alboran Sea (western Mediterranean). Stable isotopes and planktonic foraminiferal records

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reference URL

https://api.crossref.org/works/10.1016%2FS0025-3227%2898%2900020-6

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7 January 2021

based on heuristic

inferred from DOI database lookup

Identifiers

DOI

10.1016/S0025-3227(98)00020-6

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(Q58394254)

Holocene Climate Optimum and Last Glacial Maximum in the Mediterranean: the marine oxygen isotope record

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