Black Sea impact on the formation of eastern Mediterranean sapropel S1? Evidence from the Marmara Sea
暂无分享,去创建一个
[1] A. Mackensen,et al. Eastern Mediterranean surface water temperatures and delta O-18 composition during deposition of sapropels in the late Quaternary , 2003 .
[2] M. Schwarz,et al. Marine tephra from the Cape Riva eruption (22 ka) of Santorini in the Sea of Marmara , 2002 .
[3] P. Mayewski,et al. Holocene atmosphere-ocean interactions: records from Greenland and the Aegean Sea , 2002 .
[4] T. Stocker,et al. Apparent long-term cooling of the sea surface in the northeast Atlantic and Mediterranean during the Holocene. , 2002 .
[5] A. Aksu,et al. Persistent holocene outflow from the Black Sea to the eastern Mediterranean contradicts Noah's flood hypothesis , 2002 .
[6] M. Krom,et al. Nile River sediment fluctuations over the past 7000 yr and their key role in sapropel development , 2002 .
[7] M. Sperling,et al. Drying of samples may alter foraminiferal isotopic ratios and faunistic composition , 2002 .
[8] N. Shackleton,et al. Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary , 2001 .
[9] E. Rohling,et al. High-resolution geochemical and micropalaeontological profiling of the most recent eastern Mediterranean sapropel , 2001 .
[10] G. Karlık,et al. Is the abrupt drowning of the Black Sea shelf at 7150yrbp a myth , 2001 .
[11] J. Grimalt,et al. Variability of the western Mediterranean Sea surface temperature during the last 25,000 years and its connection with the Northern Hemisphere climatic changes , 2001 .
[12] J. Grimalt,et al. Evidence for enhanced Mediterranean thermohaline circulation during rapid climatic coolings , 2000 .
[13] R. Ballard,et al. Further evidence of abrupt Holocene drowning of the Black Sea shelf , 2000 .
[14] C. Eastoe,et al. Late Glacial-Holocene palaeoceanography of the Sea of Marmara: timing of connections with the Mediterranean and the Black Seas , 2000 .
[15] J. Thomson,et al. Duration of S1, the most recent sapropel in the eastern Mediterranean Sea, as indicated by accelerator mass spectrometry radiocarbon and geochemical evidence , 2000 .
[16] F. Oldfield,et al. Palaeoclimate and the Formation of Sapropel S1: Inferences from Late Quaternary Lacustrine and Marine Sequences in the Central Mediterranean Region , 2000 .
[17] K. Emeis,et al. Temperature and salinity variations of Mediterranean Sea surface waters over the last 16,000 years from records of planktonic stable oxygen isotopes and alkenone unsaturation ratios , 2000 .
[18] P. Meyers,et al. Isotopic evidence of sea-surface freshening, enhanced productivity, and improved organic matter preservation during sapropel deposition in the Tyrrhenian Sea , 2000 .
[19] E. Rohling. Paleosalinity: confidence limits and future applications , 2000 .
[20] G. Papatheodorou,et al. Evaluation of palaeoenvironmental changes during the last 18,000 years in the Myrtoon basin, SW Aegean Sea , 2000 .
[21] E. Bard,et al. Radiocarbon Reservoir Ages in the Mediterranean Sea and Black Sea , 2000, Radiocarbon.
[22] D. Stow,et al. Seismic features diagnostic of contourite drifts , 1999 .
[23] M. Rossignol-Strick. The Holocene climatic optimum and pollen records of sapropel 1 in the eastern Mediterranean, 9000–6000 BP , 1999 .
[24] A. Aksu,et al. Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea–Black Sea drainage corridor , 1999 .
[25] C. Pierre. THE OXYGEN AND CARBON ISOTOPE DISTRIBUTION IN THE MEDITERRANEAN WATER MASSES , 1999 .
[26] A. Cramp,et al. Neogene sapropels in the Mediterranean: a review , 1999 .
[27] W. Dean,et al. Organic‐matter production and preservation and evolution of anoxia in the Holocene Black Sea , 1998 .
[28] A. Rosell‐Melé,et al. Calibration of the alkenone paleotemperature index U37K′ based on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S) , 1998 .
[29] G. Bigg,et al. Paleosalinity and δ18O: A critical assessment , 1998 .
[30] J. Duplessy,et al. Temperature and salinity records of the Tyrrhenian Sea during the last 18,000 years , 1997 .
[31] F. Jorissen,et al. 200 Year interruption of Holocene sapropel formation in the Adriatic Sea , 1997, Journal of Micropalaeontology.
[32] W. Ryan,et al. An abrupt drowning of the Black Sea shelf , 1997 .
[33] Eelco J. Rohling,et al. POSTGLACIAL CONNECTION OF THE BLACK SEA TO THE MEDITERRANEAN AND ITS RELATION TO THE TIMING OF SAPROPEL FORMATION , 1997 .
[34] A. Aksu,et al. Paleoclimatic and paleoceanographic conditions leading to development of sapropel layer S1 in the Aegean Sea , 1995 .
[35] A. Aksu,et al. Late glacial-Holocene paleoclimatic and paleoceanographic evolution of the Aegean Sea: micropaleontological and stable isotopic evidence , 1995 .
[36] S. Bottema. The Younger Dryas in the Eastern Mediterranean , 1995 .
[37] E. Bard,et al. Reconstructing sea surface temperature and salinity using δ18O and alkenone records , 1993, Nature.
[38] P. Reimer,et al. Extended 14C Data Base and Revised CALIB 3.0 14C Age Calibration Program , 1993, Radiocarbon.
[39] Temel Oguz,et al. On the Physical Oceanography of the Turkish Straits , 1990 .
[40] R. Fairbanks. A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.
[41] R. Thunell,et al. Glacial–Holocene salinity changes in the Mediterranean Sea: hydrographic and depositional effects , 1989, Nature.
[42] S. Alavi. LATE HOLOCENE DEEP-SEA BENTHIC FORAMINIFERA FROM THE SEA OF MARMARA , 1988 .
[43] G. Eglinton,et al. Molecular stratigraphy: a new tool for climatic assessment , 1986, Nature.
[44] M. Rossignol-Strick. Mediterranean Quaternary sapropels, an immediate response of the african monsoon to variation of insolation , 1985 .