noaa-lake-5463
Lago Grande di Monticchio 101KYr High Resolution Sediment Data
Allen, J.R.M.; Huntley, B.; Negendank, J.F.W.
Lago Grande di Monticchio 101KYr High Resolution Sediment Data
2002-03-01
NCDC-Paleoclimatology
ONLINE Files
Pending
https://www.ncdc.noaa.gov/paleo/study/5463
Investigator
J.R.M.
Allen
Investigator
B.
Huntley
Investigator
J.F.W.
Negendank
earth science
paleoclimate
climate reconstructions|pollen
actual/potential evapotranspiration,null,null,dimensionless,null,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces; mean closest 10
earth science
paleoclimate
climate reconstructions|pollen
growing degree days,null,one standard error,kelvin day,null,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces; GDD above 5 degrees C
earth science
paleoclimate
paleolimnology
biogenic silica,sediment,null,weight percent,null,paleolimnology,null,x-ray fluorescence spectroscopy,N,normative model
earth science
paleoclimate
paleolimnology
volume magnetic susceptibility,sediment,null,dimensionless (SI system),null,paleolimnology,smoothed,null,N,x10-3 units; 3 point weighted moving average
earth science
paleoclimate
climate reconstructions|pollen
age,null,null,calendar year before present,null,climate reconstructions|pollen,null,null,N,mean closest 10
earth science
paleoclimate
paleolimnology
notes,null,null,null,null,paleolimnology,null,null,C,null
earth science
paleoclimate
climate reconstructions|pollen
temperature,null,null,degree Celsius,coldest month,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces
earth science
paleoclimate
paleolimnology
biogenic silica,sediment,null,weight percent,null,paleolimnology,corrected,x-ray fluorescence spectroscopy,N,negative values set to zero
earth science
paleoclimate
paleolimnology
depth,null,null,meter,null,paleolimnology,null,null,N,null
earth science
paleoclimate
climate reconstructions|pollen
temperature,null,one standard error,degree Celsius,coldest month,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces
earth science
paleoclimate
climate reconstructions|pollen
growing degree days,null,null,kelvin day,null,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces; GDD above 5 degrees C; mean closest 10
earth science
paleoclimate
paleolimnology
density,dry sediment,null,gram per cubic meter,null,paleolimnology,null,null,N,null
earth science
paleoclimate
paleolimnology
volume magnetic susceptibility,sediment,null,dimensionless (SI system),null,paleolimnology,null,null,N,x10-3 units
earth science
paleoclimate
climate reconstructions|pollen
actual/potential evapotranspiration,null,one standard error,dimensionless,null,climate reconstructions|pollen,null,null,N,based on pollen-climate response surfaces
earth science
paleoclimate
paleolimnology
age,null,null,calendar kiloyear before present,null,paleolimnology,null,null,N,null
earth science
paleoclimate
paleolimnology
age,null,null,calendar year before present,null,paleolimnology,null,null,N,null
earth science
paleoclimate
paleolimnology
organic matter,sediment,null,weight percent,null,paleolimnology,null,loss on ignition,N,550 degrees C
earth science
paleoclimate
paleolimnology
reconstruction
earth science
paleoclimate
paleolimnology
physical properties
earth science
paleoclimate
paleolimnology
geochemistry
earth science
paleoclimate
paleolimnology
lake level
geoscientificInformation
101768 cal yr BP
58 cal yr BP
Complete
40.93333
40.93333
15.5833
15.5833
656
656
Continent
Europe
Southern Europe
Italy
Lago Grande Di Monticchio cores B,D,J,L>LATITUDE 40.93333>LONGITUDE 15.5833
None
Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.
English
DOC/NOAA/NESDIS/NCEI
National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
https://www.ncdc.noaa.gov/data-access/paleoclimatology-data
DATA Center Contact
Bruce
Bauer
bruce.a.bauer@noaa.gov
paleo@noaa.gov
303-497-6280
303-497-6513
325 Broadway, E/NE31
Boulder
CO
80305-3328
USA
online
ASCII
Allen, J.R.M., B. Huntley, J.F.W. Negendank. 1999. Rapid environmental changes in southern Europe during the last glacial period. Nature Vol. 400, pp. 740-743, 19 Aug 1999
Oxygen-isotope records from Greenland ice cores indicate numerous rapid climate fluctuations during the last glacial period. North Atlantic marine sediment cores show comparable variability in sea surface temperature and the deposition of ice-rafted debris. In contrast, very few continental records of this time period provide the temporal resolution and environmental sensitivity necessary to reveal the extent and effects of these environmental fluctuations on the continents. Here we present high-resolution geochemical, physical and pollen data from lake sediments in Italy and from a Mediterranean sediment core, linked by a common tephrochronology. Our lacustrine sequence extends to the past 102,000 years. Many of its features correlate well with the Greenland ice-core records, demonstrating that the closely coupled ocean-atmosphere system of the Northern Hemisphere during the last glacial extended its influence at least as far as the central Mediterranean region. 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, our 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.
STUDY NOTES: Multi-proxy lacustrine sediments independantly dated by sedimentation rate based chronology corroborated by dated tephras. Linked to Mediterranean marine sediments dated by tephrochronology.
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/pollen.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/dry-density.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/allen1999.xls
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/pollen-recons.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/bio-silica.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/readme_allen1999.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/age.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/loi.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/italy/mag-sus.txt
USA/NOAA
DIF
Version 9.8.4
2018-12-11
2018-12-11