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Huang, Xianyu
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Huang, Xianyu
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland f...
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland f...
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland f...
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Characterising organic carbon sources in Anthropocene affected Arctic upland lak...
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Anthropocene climate warming enhances autochthonous carbon cycling in an upland...
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Catchment geochemical analyses from Disko 1,2 & 4 lake catchments, Disko Island...
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Catchment bulk geochemical analyses from Disko 1,2 & 4 lake catchments, Disko Is...
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Compound-specific carbon isotope analyses of samples from the Disko 2 lake catch...
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Anthropocene climate warming enhances autochthonous carbon cycling in an upland...
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Anthropocene climate warming enhances autochthonous carbon cycling in an upland...
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Catchment bulk geochemical analyses from Disko 1,2 & 4 lake catchments, Disko Is...
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Anthropocene climate warming enhances autochthonous carbon cycling in an upland...
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Characterising organic carbon sources in Anthropocene affected Arctic upland lak...
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Down-core geochemical data from Disko 2 lake sediment core (West Greenland) coll...
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Catchment geochemical analyses from Disko 1,2 & 4 lake catchments, Disko Island...
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Down-core geochemical data from Disko 2 lake sediment core (West Greenland) coll...
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Down-core geochemical data from Disko 2 lake sediment core (West Greenland) coll...
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Catchment geochemical analyses from Disko 1,2 & 4 lake catchments, Disko Island...
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Related Subjects
Arctic
Disko Island
Greenland
carbon isotope analysis
Carbon/Nitrogen ratio
Lake sediment
Disko Bay
Hand trowel
δ13C
Costech) coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer (MS)
Disko_2_lake_catchment
Element analyser CHN (ECS4010
Event label
Organic Geochemistry
Additional Funding
CLIMATE
DELTA-O-18
Disko_4_lake_catchment
EVENT
HON-Kajak sediment corer
Holocene
Hydroclimate
Latitude of event
Lipids
Longitude of event
MONSOON PRECIPITATION
Meteorology & Atmospheric Sciences
OPTIMUM
Ocean-atmospheric teleconnection
SEASONAL TRANSITIONS
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