The Sea of Marmara during Marine Isotope Stages 5 and 6
Multi-proxy analyses and lithology of two cores, MRS-CS18 and MRS-CS27, from the İmralı Basin of the Sea of Marmara (SoM) provide novel information on environmental conditions, relative sea level, and sill depths of the straits of Bosporus and Dardanelles during the Marine Isotope Stages (MIS) 5 and...
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| Veröffentlicht in: | Quaternary science reviews 2019-09, Vol.220, p.124-141 |
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| creator | Çağatay, M. Namık Eriş, K. Kadir Makaroğlu, Özlem Yakupoğlu, Nurettin Henry, Pierre Leroy, Suzanne A.G. Uçarkuş, Gülsen Sakınç, Mehmet Yalamaz, Burak Bozyiğit, Cerennaz Kende, Julia |
| description | Multi-proxy analyses and lithology of two cores, MRS-CS18 and MRS-CS27, from the İmralı Basin of the Sea of Marmara (SoM) provide novel information on environmental conditions, relative sea level, and sill depths of the straits of Bosporus and Dardanelles during the Marine Isotope Stages (MIS) 5 and 6. The fossil and multi-proxy geochemical records show that lacustrine conditions prevailed in the SoM during most of MIS 6, from 171 to 134 ka BP, and that the transition to marine conditions during Termination II took place at ∼134.06 ± 1.10 ka BP. MIS 5 interstadials a, c, and e witnessed the formation of three sapropels (MSAP-2, MSAP-3 and MSAP-4) under suboxic to anoxic marine conditions, whereas during stadials MIS 5b (∼94–86) and MIS 5d (∼112–105 ka BP), lacustrine and marine conditions with deposition of sediments having relatively low TOC contents ( |
| doi_str_mv | 10.1016/j.quascirev.2019.07.031 |
| format | Article |
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The SoM geochemical proxy records correlate well with the regional terrestrial and marine records and the NGRIP oxygen isotope record with its Stadial and Interstadial phases, showing the common effect of the North Atlantic climatic events triggered by the perturbations in the Atlantic Meridional Overturning Circulation. However, the amplitude of the oscillations recorded in the SoM during MIS 6 (Penultimate Glacial Period) is relatively small compared to the MIS 4 to MIS 2 (Last Glacial Period).
•First paper to discuss the paleoceanography of an important gateway during MIS 5 and MIS 6.•First complete documentation of MIS 5 sapropels and their origin.•Sea/water level changes and timing of marine connection during Termination II.•Correlation of the Sea of Marmara records with regional and global records.•Reporting of a new unidentified tephra.</description><identifier>ISSN: 0277-3791</identifier><identifier>EISSN: 1873-457X</identifier><identifier>DOI: 10.1016/j.quascirev.2019.07.031</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Earth Sciences ; Eastern Europe ; Geochemical proxies ; Geochemistry ; Late quaternary ; Marine isotope stages 5–6 ; Paleoceanography ; Sapropels ; Sciences of the Universe ; Sea of Marmara ; Sedimentology-marine cores ; Stratigraphy</subject><ispartof>Quaternary science reviews, 2019-09, Vol.220, p.124-141</ispartof><rights>2019 Elsevier Ltd</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a421t-a0cc5a86931c0e29be11a2d5a768aae6f36e34fa00e3883cd28cb6e853ac26993</citedby><cites>FETCH-LOGICAL-a421t-a0cc5a86931c0e29be11a2d5a768aae6f36e34fa00e3883cd28cb6e853ac26993</cites><orcidid>0000-0002-2288-6805 ; 0000-0002-2556-2339</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0277379119304998$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,27901,27902,65534</link.rule.ids><backlink>$$Uhttps://hal.science/hal-02415856$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Çağatay, M. Namık</creatorcontrib><creatorcontrib>Eriş, K. Kadir</creatorcontrib><creatorcontrib>Makaroğlu, Özlem</creatorcontrib><creatorcontrib>Yakupoğlu, Nurettin</creatorcontrib><creatorcontrib>Henry, Pierre</creatorcontrib><creatorcontrib>Leroy, Suzanne A.G.</creatorcontrib><creatorcontrib>Uçarkuş, Gülsen</creatorcontrib><creatorcontrib>Sakınç, Mehmet</creatorcontrib><creatorcontrib>Yalamaz, Burak</creatorcontrib><creatorcontrib>Bozyiğit, Cerennaz</creatorcontrib><creatorcontrib>Kende, Julia</creatorcontrib><title>The Sea of Marmara during Marine Isotope Stages 5 and 6</title><title>Quaternary science reviews</title><description>Multi-proxy analyses and lithology of two cores, MRS-CS18 and MRS-CS27, from the İmralı Basin of the Sea of Marmara (SoM) provide novel information on environmental conditions, relative sea level, and sill depths of the straits of Bosporus and Dardanelles during the Marine Isotope Stages (MIS) 5 and 6. The fossil and multi-proxy geochemical records show that lacustrine conditions prevailed in the SoM during most of MIS 6, from 171 to 134 ka BP, and that the transition to marine conditions during Termination II took place at ∼134.06 ± 1.10 ka BP. MIS 5 interstadials a, c, and e witnessed the formation of three sapropels (MSAP-2, MSAP-3 and MSAP-4) under suboxic to anoxic marine conditions, whereas during stadials MIS 5b (∼94–86) and MIS 5d (∼112–105 ka BP), lacustrine and marine conditions with deposition of sediments having relatively low TOC contents (<2%) prevailed, respectively. Consideration of the global sea level, together with the timing of the marine reconnection of the SoM during Termination II and persistence of the marine conditions during MIS 5, except for MIS 5b and later part of MIS 5a, suggests that the Dardanelles sill depth was at ∼ -75 ± 5 m during the reconnection at Termination II and at −55 ± 5 m during most of MIS 5. On similar considerations of the Black Sea marine reconnections and disruptions during the MIS 5, a sill depth of −35 to −40 m (similar to the present day depth) is indicated for the Bosporus Strait.
The SoM geochemical proxy records correlate well with the regional terrestrial and marine records and the NGRIP oxygen isotope record with its Stadial and Interstadial phases, showing the common effect of the North Atlantic climatic events triggered by the perturbations in the Atlantic Meridional Overturning Circulation. However, the amplitude of the oscillations recorded in the SoM during MIS 6 (Penultimate Glacial Period) is relatively small compared to the MIS 4 to MIS 2 (Last Glacial Period).
•First paper to discuss the paleoceanography of an important gateway during MIS 5 and MIS 6.•First complete documentation of MIS 5 sapropels and their origin.•Sea/water level changes and timing of marine connection during Termination II.•Correlation of the Sea of Marmara records with regional and global records.•Reporting of a new unidentified tephra.</description><subject>Earth Sciences</subject><subject>Eastern Europe</subject><subject>Geochemical proxies</subject><subject>Geochemistry</subject><subject>Late quaternary</subject><subject>Marine isotope stages 5–6</subject><subject>Paleoceanography</subject><subject>Sapropels</subject><subject>Sciences of the Universe</subject><subject>Sea of Marmara</subject><subject>Sedimentology-marine cores</subject><subject>Stratigraphy</subject><issn>0277-3791</issn><issn>1873-457X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNqFkE1Lw0AQhhdRsFZ_g3v1kLgf2Y8cS1FbqHiwgrdlupm0KTWpu2nBf--GSq-ehhmed5h5CLnnLOeM68dt_n2A6JuAx1wwXubM5EzyCzLi1sisUObzkoyYMCaTpuTX5CbGLWNMCStGxCw3SN8RaFfTVwhfEIBWh9C066FtWqTz2PXdPkE9rDFSRaGtqL4lVzXsIt791TH5eH5aTmfZ4u1lPp0sMigE7zNg3iuwupTcMxTlCjkHUSkw2gKgrqVGWdTAGEprpa-E9SuNVknwQpelHJOH094N7Nw-NOnAH9dB42aThRtmTBRcWaWPPLHmxPrQxRiwPgc4c4Mrt3VnV25w5ZhxyVVKTk5JTK8cGwwuQdh6rBLqe1d1zb87fgGk53Tn</recordid><startdate>20190915</startdate><enddate>20190915</enddate><creator>Çağatay, M. Namık</creator><creator>Eriş, K. Kadir</creator><creator>Makaroğlu, Özlem</creator><creator>Yakupoğlu, Nurettin</creator><creator>Henry, Pierre</creator><creator>Leroy, Suzanne A.G.</creator><creator>Uçarkuş, Gülsen</creator><creator>Sakınç, Mehmet</creator><creator>Yalamaz, Burak</creator><creator>Bozyiğit, Cerennaz</creator><creator>Kende, Julia</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0002-2288-6805</orcidid><orcidid>https://orcid.org/0000-0002-2556-2339</orcidid></search><sort><creationdate>20190915</creationdate><title>The Sea of Marmara during Marine Isotope Stages 5 and 6</title><author>Çağatay, M. Namık ; Eriş, K. Kadir ; Makaroğlu, Özlem ; Yakupoğlu, Nurettin ; Henry, Pierre ; Leroy, Suzanne A.G. ; Uçarkuş, Gülsen ; Sakınç, Mehmet ; Yalamaz, Burak ; Bozyiğit, Cerennaz ; Kende, Julia</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a421t-a0cc5a86931c0e29be11a2d5a768aae6f36e34fa00e3883cd28cb6e853ac26993</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Earth Sciences</topic><topic>Eastern Europe</topic><topic>Geochemical proxies</topic><topic>Geochemistry</topic><topic>Late quaternary</topic><topic>Marine isotope stages 5–6</topic><topic>Paleoceanography</topic><topic>Sapropels</topic><topic>Sciences of the Universe</topic><topic>Sea of Marmara</topic><topic>Sedimentology-marine cores</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Çağatay, M. Namık</creatorcontrib><creatorcontrib>Eriş, K. Kadir</creatorcontrib><creatorcontrib>Makaroğlu, Özlem</creatorcontrib><creatorcontrib>Yakupoğlu, Nurettin</creatorcontrib><creatorcontrib>Henry, Pierre</creatorcontrib><creatorcontrib>Leroy, Suzanne A.G.</creatorcontrib><creatorcontrib>Uçarkuş, Gülsen</creatorcontrib><creatorcontrib>Sakınç, Mehmet</creatorcontrib><creatorcontrib>Yalamaz, Burak</creatorcontrib><creatorcontrib>Bozyiğit, Cerennaz</creatorcontrib><creatorcontrib>Kende, Julia</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Quaternary science reviews</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Çağatay, M. Namık</au><au>Eriş, K. Kadir</au><au>Makaroğlu, Özlem</au><au>Yakupoğlu, Nurettin</au><au>Henry, Pierre</au><au>Leroy, Suzanne A.G.</au><au>Uçarkuş, Gülsen</au><au>Sakınç, Mehmet</au><au>Yalamaz, Burak</au><au>Bozyiğit, Cerennaz</au><au>Kende, Julia</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Sea of Marmara during Marine Isotope Stages 5 and 6</atitle><jtitle>Quaternary science reviews</jtitle><date>2019-09-15</date><risdate>2019</risdate><volume>220</volume><spage>124</spage><epage>141</epage><pages>124-141</pages><issn>0277-3791</issn><eissn>1873-457X</eissn><abstract>Multi-proxy analyses and lithology of two cores, MRS-CS18 and MRS-CS27, from the İmralı Basin of the Sea of Marmara (SoM) provide novel information on environmental conditions, relative sea level, and sill depths of the straits of Bosporus and Dardanelles during the Marine Isotope Stages (MIS) 5 and 6. The fossil and multi-proxy geochemical records show that lacustrine conditions prevailed in the SoM during most of MIS 6, from 171 to 134 ka BP, and that the transition to marine conditions during Termination II took place at ∼134.06 ± 1.10 ka BP. MIS 5 interstadials a, c, and e witnessed the formation of three sapropels (MSAP-2, MSAP-3 and MSAP-4) under suboxic to anoxic marine conditions, whereas during stadials MIS 5b (∼94–86) and MIS 5d (∼112–105 ka BP), lacustrine and marine conditions with deposition of sediments having relatively low TOC contents (<2%) prevailed, respectively. Consideration of the global sea level, together with the timing of the marine reconnection of the SoM during Termination II and persistence of the marine conditions during MIS 5, except for MIS 5b and later part of MIS 5a, suggests that the Dardanelles sill depth was at ∼ -75 ± 5 m during the reconnection at Termination II and at −55 ± 5 m during most of MIS 5. On similar considerations of the Black Sea marine reconnections and disruptions during the MIS 5, a sill depth of −35 to −40 m (similar to the present day depth) is indicated for the Bosporus Strait.
The SoM geochemical proxy records correlate well with the regional terrestrial and marine records and the NGRIP oxygen isotope record with its Stadial and Interstadial phases, showing the common effect of the North Atlantic climatic events triggered by the perturbations in the Atlantic Meridional Overturning Circulation. However, the amplitude of the oscillations recorded in the SoM during MIS 6 (Penultimate Glacial Period) is relatively small compared to the MIS 4 to MIS 2 (Last Glacial Period).
•First paper to discuss the paleoceanography of an important gateway during MIS 5 and MIS 6.•First complete documentation of MIS 5 sapropels and their origin.•Sea/water level changes and timing of marine connection during Termination II.•Correlation of the Sea of Marmara records with regional and global records.•Reporting of a new unidentified tephra.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.quascirev.2019.07.031</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-2288-6805</orcidid><orcidid>https://orcid.org/0000-0002-2556-2339</orcidid><oa>free_for_read</oa></addata></record> |
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| language | eng |
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| source | Elsevier ScienceDirect Journals Complete |
| subjects | Earth Sciences Eastern Europe Geochemical proxies Geochemistry Late quaternary Marine isotope stages 5–6 Paleoceanography Sapropels Sciences of the Universe Sea of Marmara Sedimentology-marine cores Stratigraphy |
| title | The Sea of Marmara during Marine Isotope Stages 5 and 6 |
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