Last glacial–Holocene paleoceanography of the Black Sea and Marmara Sea: stable isotopic, foraminiferal and coccolith evidence

Autor: Aksu, A.E., Hiscott, R.N., Kaminski, M.A., Mudie, P.J., Gillespie, H., Abrajano, T., Yaşar, D.

Publikováno v: In Marine Geology 2002 190(1):119-149

Isotopic fractionation of carbon and chlorine by microbial degradation of dichloromethane

Autor: Heraty, L.J ^*, Fuller, M.E, Huang, L, Abrajano, T, Jr, Sturchio, N.C

Publikováno v: In Organic Geochemistry 1999 30(8) Part 1:793-799

Carbon isotopic fractionation during reductive dehalogenation of chlorinated ethenes by metallic iron

Autor: Dayan, H, Abrajano, T ^*, Sturchio, N.C, Winsor, L

Publikováno v: In Organic Geochemistry 1999 30(8) Part 1:755-763

The Marmara Sea Gateway since ~16 ky BP: non-catastrophic causes of paleoceanographic events in the Black Sea at 8.4 and 7.15 ky BP

Autor: Hiscott, R. N., Aksu, A. E., Mudie, P. J., Kaminski, M. A., Abrajano, T., Yaşar, D., Rochon, A.

Publikováno v: Yanko-Hombach, V. and Gilbert, A.S. and Panin, N. and Dolukhanov, P.M., (eds.) The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement. (pp. 89-118). Springer: Dordrecht, The Netherlands. (2007)

The Late Quaternary history of connection of the Black Sea to the Eastern Mediterranean has been intensely debated. Ryan, Pitman and coworkers advocate two pulses of outflow from the Black Sea to the world ocean at ~16–14.7 ky BP and ~11–10 ky BP

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______322::00ea692e3c91b02d68dea1cedab384bb
https://discovery.ucl.ac.uk/id/eprint/18638/

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