Hydrological conditions over the western Mediterranean basin during the deposition of the cold Sapropel 6 (ca. 175 kyr BP)

• Published in: Earth and planetary science letters 2002-09, Vol.202 (2), p.481-494
• Main Authors: Bard, Edouard, Delaygue, Gilles, Rostek, Frauke, Antonioli, Fabrizio, Silenzi, Sergio, Schrag, Daniel P.
• Format: Article
• Language: English
• Subjects: Bioclimatology; Ecology, environment; Freshwater; Life Sciences; Marine; Mediterranean Sea; modeling of oxygen isotopes; paleoclimatology; sapropels; speleothems
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/S0012-821X(02)00788-4

A new oxygen isotope record is reported from a stalagmite collected in the Argentarola Cave located on the Tyrrhenian coast of Italy. As shown from observations and numerical modeling of δ 18O in modern precipitation, the recorded δ 18O variability for this zone is dominated by the amount of precipitation (so-called ‘amount effect’). The δ 18O profile measured in the stalagmite is characterized by a prominent negative excursion (ca. 2–3‰) between 180 and 170 kyr BP. This paleoclimatic feature is interpreted as being due to a relatively wet period which occurred during the penultimate glacial period, more precisely, during Marine Isotope Stage 6.5. This pluvial phase is shown to correspond chronologically to the deposition of the sapropel event 6 (S6). Although this particular sapropel event occurred during a cold phase, the δ 18O excursion is similar to those corresponding to other sapropels (S4, S3 and S2). The evidence for humid conditions during S6 in the western Mediterranean basin agrees with previous studies based on deep-sea sediment cores. Taken collectively, the data suggest that during sapropel events dilution of ocean surface waters was not restricted to the output of the river Nile but was rather widespread over the entire Mediterranean Sea due to increased rainfall.