Here we use compound-specific hydrogen isotope data of aquatic and terrestrial lipid biomarkers from precisely dated annually laminated sediments from Lake Meerfelder Maar (MFM) in Western Germany to reconstruct decadal resolved hydroclimatic changes during the Younger Dryas. We show that cooling at MFM begun synchronous to the onset of cooling in Greenland at 12.850 years BP. Major environmental changes at MFM however took place 170 years later as a result of substantially drier conditions
In this thesis, the late glacial climate and environment development with special focus on the Young...
We present a hydrogen isotopic record of long-chain n-alkanes in Lake Sugan to reconstruct regional ...
The response of a lacustrine ecosystem to climatic changes from 13,500 to 10,800 BP was studied in a...
Abstract The regional patterns and timing of the Younger Dryas cooling in the North Atlantic realm ...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
The Younger Dryas was the final cold phase during the last deglaciation; it started with an abrupt c...
Causes of the Late Glacial to Early Holocene transition phase and particularly the Younger Dryas per...
We reconstructed middle to late Holocene changes in atmospheric circulation patterns and vegetation ...
A lake sediment record from the Friedla¨nder Grobe Wiese in northeast Germany was studied to recons...
We reconstructed middle to late Holocene changes in atmospheric circulation patterns and vegetation ...
Recent successful drilling operations at Lake El\u27gygytgyn, NE Russia have recovered sediment core...
Ice core records have long indicated that the Younger Dryas began and ended with large, abrupt clima...
Recent successful drilling operations at Lake El\u27gygytgyn, NE Russia have recovered sediment core...
In this thesis, the late glacial climate and environment development with special focus on the Young...
We present a hydrogen isotopic record of long-chain n-alkanes in Lake Sugan to reconstruct regional ...
The response of a lacustrine ecosystem to climatic changes from 13,500 to 10,800 BP was studied in a...
Abstract The regional patterns and timing of the Younger Dryas cooling in the North Atlantic realm ...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler...
The Younger Dryas was the final cold phase during the last deglaciation; it started with an abrupt c...
Causes of the Late Glacial to Early Holocene transition phase and particularly the Younger Dryas per...
We reconstructed middle to late Holocene changes in atmospheric circulation patterns and vegetation ...
A lake sediment record from the Friedla¨nder Grobe Wiese in northeast Germany was studied to recons...
We reconstructed middle to late Holocene changes in atmospheric circulation patterns and vegetation ...
Recent successful drilling operations at Lake El\u27gygytgyn, NE Russia have recovered sediment core...
Ice core records have long indicated that the Younger Dryas began and ended with large, abrupt clima...
Recent successful drilling operations at Lake El\u27gygytgyn, NE Russia have recovered sediment core...
In this thesis, the late glacial climate and environment development with special focus on the Young...
We present a hydrogen isotopic record of long-chain n-alkanes in Lake Sugan to reconstruct regional ...
The response of a lacustrine ecosystem to climatic changes from 13,500 to 10,800 BP was studied in a...