Dinocyst assemblages and water surface conditions in the Sea of Marmara during MIS 6 and 5 from two long cores

Autor: Leroy, S.A.G., Henry, P., Marret, F., Pailles, C., Licari, L., Kende, J., Rostek, F., Bard, E.

Publikováno v: In Quaternary Science Reviews 15 August 2023 314

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Hydrology in the Sea of Marmara during the last 23 ka: Implications for timing of Black Sea connections and sapropel deposition

Autor: Vidal, L., Ménot, G., Joly, C., Bruneton, H., Rostek, F., Çağatay, M. N., Major, C., Bard, E.

Publikováno v: Paleoceanography (0883-8305) (Amer Geophysical Union), 2010-02, Vol. 25, N. 1 / PA1205, P. 1-16
Paleoceanography
Paleoceanography, 2010, 25 (1), ⟨10.1029/2009PA001735⟩

Sediments deposited under lacustrine and marine conditions in the Sea of Marmara hold a Late Quaternary record for water exchange between the Black Sea and the Mediterranean Sea. Here we report a multiproxy data set based on oxygen and strontium isot

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0644d67612153b48ee1e94efc59ecbcd
https://archimer.ifremer.fr/doc/00231/34243/

Western Arabian Sea SST during the penultimate interglacial: A comparison of U_37 ^K' and Mg/Ca paleothermometry

Autor: Saher, M.H., Rostek, F., Jung, S.J.A., Bard, E, Schneider, R.R., Greaves, M., Ganssen, G.M., Elderfield, H., Kroon, D.

Publikováno v: Saher, M H, Rostek, F, Jung, S J A, Bard, E, Schneider, R R, Greaves, M, Ganssen, G M, Elderfield, H & Kroon, D 2009, ' Western Arabian Sea SST during the penultimate interglacial: A comparison of U_37 ^K' and Mg/Ca paleothermometry ', Paleoceanography, vol. 24, pp. PA2212 . https://doi.org/10.1029/2007PA001557
Saher, M H, Rostek, F, Jung, S, Bard, E, Schneider, R R, Greaves, M, Ganssen, G M, Elderfield, H & Kroon, D 2009, ' Western Arabian Sea SST during the penultimate interglacial: A comparison of U-37(K ') and Mg/Ca paleothermometry ', Paleoceanography, vol. 24 . https://doi.org/10.1029/2007PA001557
Paleoceanography, 24. American Geophysical Union

Millennial-scale records of planktonic foraminiferal Mg/Ca, bulk sediment U37 K′, and planktonic foraminiferal δ 18O are presented across the last two deglaciations in sediment core NIOP929 from the Arabian Sea. Mg/Ca-derived temperature variabili

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9155e38832f6785351b4d5b4a3cb9de8
https://research.vu.nl/en/publications/1a248dc5-dd08-4025-a1a0-eeeba7d784c8