Younger Dryas–Holocene temperature and rainfall history of southern Indonesia from δ18O in speleothem calcite and fluid inclusions
about
Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Measurement of δ18O and δ2H values of fluid inclusion water in speleothems using cavity ring-down spectroscopy compared with isotope ratio mass spectrometry.The influence of Indian Ocean atmospheric circulation on Warm Pool hydroclimate during the Holocene epochIndonesian vegetation response to changes in rainfall seasonality over the past 25,000 yearsUsing the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciationVariability of Indonesian Throughflow and Borneo Runoff During the Last 14 kyr
P2860
Younger Dryas–Holocene temperature and rainfall history of southern Indonesia from δ18O in speleothem calcite and fluid inclusions
description
im Juni 2010 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2010
@uk
name
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@en
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@nl
type
label
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@en
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@nl
prefLabel
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@en
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@nl
P2093
P50
P1476
Younger Dryas–Holocene tempera ...... m calcite and fluid inclusions
@en
P2093
Bambang W. Suwargadi
Hubert B. Vonhof
Linda K. Ayliffe
Michael K. Gagan
Michael L. Griffiths
Russell N. Drysdale
Wahyoe S. Hantoro
P356
10.1016/J.EPSL.2010.03.018
P407
P577
2010-06-01T00:00:00Z