Worldwide acceleration of mountain erosion under a cooling climate.
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A bottom-up perspective on ecosystem change in Mesozoic oceansThe rise of ocean giants: maximum body size in Cenozoic marine mammals as an indicator for productivity in the Pacific and Atlantic OceansFrost for the trees: Did climate increase erosion in unglaciated landscapes during the late Pleistocene?Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age.A seven-million-year hornblende mineral record from the central Chinese Loess Plateau.Tectonic control on the persistence of glacially sculpted topography.Rapid sequestration of rock avalanche deposits within glaciers.Erosion by an Alpine glacier.Comment (2) on "Formation of the Isthmus of Panama" by O'Dea et alTime scale bias in erosion rates of glaciated landscapes.Ice sheets as a missing source of silica to the polar oceans.Glacial weathering, sulfide oxidation, and global carbon cycle feedbacks.Mountain glaciation drives rapid oxidation of rock-bound organic carbon.Earth science: River incision revisited.Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, northwestern China.Northward migration of the eastern Himalayan syntaxis revealed by OSL thermochronometry.A Pleistocene ice core record of atmospheric O2 concentrations.Widespread erosion on high plateaus during recent glaciations in Scandinavia.Geochemistry: How rain affects rock and rivers.Earth science: Erosion by cooling.Deglaciation and glacial erosion: A joint control on magma productivity by continental unloadingEffects of primitive photosynthesis on Earth’s early climate systemGlacial Steady State Topography Controlled by the Coupled Influence of Tectonics and ClimateThe role of uplift and erosion in the persistence of saline groundwater in the shallow subsurfaceHigh-resolution evolution of terrigenous sediment yields in the Provence Basin during the last 6 Ma: relation with climate and tectonicsThe null hypothesis: globally steady rates of erosion, weathering fluxes and shelf sediment accumulation during Late Cenozoic mountain uplift and glaciationModes of extensional faulting controlled by surface processesThe geomorphology of the Anthropocene: emergence, status and implicationsPhanerozoic surface history of southern Peninsular India from apatite (U-Th-Sm)/He dataLate Miocene northward propagation of the northeast Pamir thrust system, northwest ChinaUnderstanding erosion rates in the Himalayan orogen: A case study from the Arun ValleyChanging exhumation patterns during Cenozoic growth and glaciation of the Alaska Range: Insights from detrital thermochronology and geochronologyDebate articles: have changes in Quaternary climate affected erosion?
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P2860
Worldwide acceleration of mountain erosion under a cooling climate.
description
2013 nî lūn-bûn
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2013年の論文
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2013年学术文章
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2013年学术文章
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2013年学术文章
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2013年学术文章
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2013年学术文章
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2013年學術文章
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name
Worldwide acceleration of mountain erosion under a cooling climate.
@en
Worldwide acceleration of mountain erosion under a cooling climate.
@nl
type
label
Worldwide acceleration of mountain erosion under a cooling climate.
@en
Worldwide acceleration of mountain erosion under a cooling climate.
@nl
prefLabel
Worldwide acceleration of mountain erosion under a cooling climate.
@en
Worldwide acceleration of mountain erosion under a cooling climate.
@nl
P2093
P2860
P50
P356
P1433
P1476
Worldwide acceleration of mountain erosion under a cooling climate.
@en
P2093
Diane Seward
Frédéric Herman
Pierre G Valla
Sean D Willett
P2860
P2888
P304
P356
10.1038/NATURE12877
P407
P577
2013-12-01T00:00:00Z
P6179
1019838149