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Journal of Quaternary Science / Cave bear occupation in Schwabenreith Cave, Aust...
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Holocene climate variability in Central Germany and a potential link to the pola...
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Cryogenic calcites - a novel archive of continental climate during glacial phase...
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Climate spectrum estimation in the presence of timescale errors
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Climate spectrum estimation in the presence of timescale errors
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Caribbean hydroclimate and vegetation history across the last glacial period
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Climate spectrum estimation in the presence of timescale errors
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Climate spectrum estimation in the presence of timescale errors.
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Climate Variability in Central Europe during the Last 2500 Years Reconstructed f...
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Climate and structure of the 8.2 ka event reconstructed from three speleothems f...
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Last interglacial temperature seasonality reconstructed from tropical Atlantic c...
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Coarsely crystalline cryogenic cave carbonate - a new archive to estimate the La...
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Increased seasonality in Middle East temperatures during the last interglacial p...
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Climate and structure of the 8.2 ka event reconstructed from three speleothems f...
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Climate Variability in Central Europe during the Last 2500 Years Reconstructed f...
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Climate and structure of the 8.2 ka event reconstructed from three speleothems f...
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Climate Variability in Central Europe during the Last 2500 Years Reconstructed f...
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A sequence of abrupt climatic fluctuations in the north-eastern Caribbean relate...
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Holocene climate variability in north-eastern Italy: potential influence of the...
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Tropical Atlantic temperature seasonality at the end of the last interglacial
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Verlagsveröffentlichung
article
ASIAN MONSOON
ATMOSPHERIC CIRCULATION
DELTA-O-18 WATER ISOTOPE
GENERAL-CIRCULATION MODEL
GROWTH FREQUENCY VARIATIONS
HIGH-RESOLUTION
NORTH-ATLANTIC
OXYGEN-ISOTOPE
PMIP4 CONTRIBUTION
STABLE-ISOTOPE VARIATIONS
geo
550 Earth sciences & geology
Holocene
caves
envir
permafrost
speleothem
230Th
8.2 ka event
AMOC
Central America
Earth Sciences
Eastern Alps
FOS Physical sciences
Geology
Geophysics physics.geo-ph
Geosciences
Glaciology
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