The isotopic geochemistry of speleothems—I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators
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Development and disintegration of Maya political systems in response to climate change.Rapid interhemispheric climate links via the Australasian monsoon during the last deglaciation.Australian tropical cyclone activity lower than at any time over the past 550-1,500 years.Formation of amorphous calcium carbonate in caves and its implications for speleothem research.Reconciliation of the Devils Hole climate record with orbital forcingThe Asian monsoon over the past 640,000 years and ice age terminations.Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum.Climate response to the 8.2 ka event in coastal CaliforniaCyclic precipitation variation on the western Loess Plateau of China during the past four centuries.Interglacial hydroclimate in the tropical West Pacific through the Late Pleistocene.Mid-latitude interhemispheric hydrologic seesaw over the past 550,000 years.Onset and duration of transitions into Greenland Interstadials 15.2 and 14 in northern China constrained by an annually laminated stalagmite.Western Pacific hydroclimate linked to global climate variability over the past two millennia.Climate variations of Central Asia on orbital to millennial timescales.Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil.The East Asian summer monsoon variability over the last 145 years inferred from the Shihua Cave record, North China.High-latitude forcing of the South American summer monsoon during the Last Glacial.Hydroclimate changes across the Amazon lowlands over the past 45,000 years.Contribution of carbonate weathering to the CO2 efflux from temperate forest soils.An 80 kyr-long continuous speleothem record from Dim Cave, SW Turkey with paleoclimatic implications for the Eastern MediterraneanEmpirical equations for the temperature dependence of calcite-water oxygen isotope fractionation from 10 to 70°C.Characterization of the water chemistry, sediment (13)C and (18)O compositions of Kolleru Lake-a Ramsar wetland in Andhra Pradesh, India.1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene.C and O stable isotopic signatures of fast-growing dripstones on alkaline substrates: reflection of growth mechanism, carbonate sources and environmental conditions.Ice age terminations.Late Quaternary Paleoclimate in the Eastern Mediterranean Region from Stable Isotope Analysis of Speleothems at Soreq Cave, IsraelA multiple cave deposit assessment of suitability of speleothem isotopes for reconstructing palaeo-vegetation and palaeo-temperatureA Speleothem Record of Younger Dryas Cooling, Klamath Mountains, Oregon, USAThe Hekla 3 volcanic eruption recorded in a Scottish speleothem?A 230 ka record of glacial and interglacial events from Aurora Cave, Fiordland, New ZealandPaleoclimate reconstruction in the Levant region from the geochemistry of a Holocene stalagmite from the Jeita cave, LebanonSpeleothem master chronologies: combined Holocene 18O and 13C records from the North Island of New Zealand and their palaeoenvironmental interpretationDecreasing monsoon precipitation in southwest China during the last 240 years associated with the warming of tropical oceanLarge variations of δ13C values in stalagmites from southeastern China during historical times: implications for anthropogenic deforestationThe climatic cyclicity in semiarid-arid central Asia over the past 500,000 yearsCentennial- to decadal-scale monsoon precipitation variability in the semi-humid region, northern China during the last 1860 years: Records from stalagmites in Huangye CaveCarbon Cycling in Floodplain Ecosystems: Out-Gassing and Photosynthesis Transmit Soil δ13C Gradient Through Stream Food WebsA continuous stable isotope record from the penultimate glacial maximum to the Last Interglacial (159–121 ka) from Tana Che Urla Cave (Apuan Alps, central Italy)Water isotopic variability in Mallorca: a path to understanding past changes in hydroclimateComposition and sources of lipid compounds in speleothem calcite from southwestern Oregon and their paleoenvironmental implications
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The isotopic geochemistry of speleothems—I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators
description
article
@en
im August 1971 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в серпні 1971
@uk
ലേഖനം
@ml
name
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@en
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@nl
type
label
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@en
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@nl
prefLabel
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@en
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@nl
P1476
The isotopic geochemistry of s ...... y as palaeoclimatic indicators
@en
P2093
P304
P356
10.1016/0016-7037(71)90127-X
P577
1971-08-01T00:00:00Z