Lago Grande di Monticchio High Resolution Sediment Data: Readme file ----------------------------------------------------------------------- World Data Center for Paleoclimatology, Boulder and NOAA Paleoclimatology Program ----------------------------------------------------------------------- NOTE: PLEASE CITE CONTRIBUTORS WHEN USING THIS DATA!!!!! NAME OF DATA SET: Lago Grande di Monticchio High Resolution Sediment Data LAST UPDATE: 3/2002 (Original Receipt by WDC Paleo) CONTRIBUTORS: Brian Huntley, University of Durham, U.K., and Jörg F.W. Negendank, GFZ-Potsdam, Germany. IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 2002-013 SUGGESTED DATA CITATION: Allen, J.R.M., et al., 2002, Lago Grande di Monticchio High Resolution Sediment Data, IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2002-013. NOAA/NGDC Paleoclimatology Program, Boulder CO, USA. ORIGINAL REFERENCE: Allen, Judy R. M., Ute Brandt, Achim Brauer, Hans-Wolfgang Hubberten, Brian Huntley, Jörg Keller, Michael Kraml, Andreas Mackensen, Jens Mingram, Jörg F. W. Negendank, Norbert R. Nowaczyk, Hedi Oberhänsli, William A. Watts, Sabine Wulf, and Bernd Zolitschka, 1999, Rapid environmental changes in southern Europe during the last glacial period. Nature 400: 740-743 (19 Aug 1999). GEOGRAPHIC REGION: Southern Europe and Mediterranean Sea PERIOD OF RECORD: Last Glacial Period, 101 KYrBP - Present LIST OF FILES: Readme_allen1999.txt (this file), allen1999.xls (Microsoft Excel format), age.txt, bio-silica.txt, dry-density.txt, loi.txt, mag-sus.txt, meteor-iso.txt, pollen.txt, pollen-recons.txt (tab-delimited text files). DESCRIPTION: Allen et al. 1999 Lago Grande di Monticchio High Resolution Sediment Data. Multi-proxy lacustrine sediments independantly dated by sedimentation rate based chronology corroborated by dated tephras. Linked to Mediterranean marine sediments dated by tephrochronology. A series of four sediment cores (B, D, J and L) obtained from Lago Grande di Monticchio (40° 56' N, 15° 35' E, 656 m above sea level), a maar lake in Basilicata, southern Italy, extend to a depth of 72.5 m, and are independantly dated (sedimentation rate based chronology) to 102,000 years. Numerous vegetation changes were rapid, frequently occurring in less than 200 years, showing that the terrestrial biosphere participated fully in last-glacial climate variability. Earlier than 65,000 years ago, the record shows more climate fluctuations than are apparent in the Greenland ice cores. Together, the multi-proxy data from the continental and marine records reveal differences in the seasonal character of climate during successive interstadials, and provide a step towards determining the underlying mechanisms of the centennial-millennial-scale variability.