Climate change as the dominant control on glacial-interglacial variations in C3 and C4 plant abundance.
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Responses of Amazonian ecosystems to climatic and atmospheric carbon dioxide changes since the last glacial maximumNature's green revolution: the remarkable evolutionary rise of C4 plantsCrystal structure of the MexR repressor of the mexRAB-oprM multidrug efflux operon of Pseudomonas aeruginosaSeaweeds in cold seas: evolution and carbon acquisitionEcosystem variability and early human habitats in eastern AfricaEvolution of mammals and their gut microbesHistorical climate change and speciation: neotropical seasonally dry forest plants show patterns of both tertiary and quaternary diversificationDrought, agricultural adaptation, and sociopolitical collapse in the Maya LowlandsExtended megadroughts in the southwestern United States during Pleistocene interglacials.A late-Quaternary perspective, on atmospheric pCO2, climate, and fire as drivers of C4-grass abundance.African vegetation controlled by tropical sea surface temperatures in the mid-Pleistocene period.Reconstructing vapor pressure deficit from leaf wax lipid molecular distributions.The evolution of C4photosynthesisPalaeozoological insights into management options for a threatened mammal: southern Africa’s Cape mountain zebra (Equus zebra zebra)Climate and CO2 controls on global vegetation distribution at the last glacial maximum: analysis based on palaeovegetation data, biome modelling and palaeoclimate simulationsStable carbon isotopes (δ13C) of total organic carbon and long-chain n-alkanes as proxies for climate and environmental change in a sediment core from Lake Petén-Itzá, GuatemalaNeotropical C3/C4 grass distributions - present, past and futureLeaf area index for northern and eastern North America at the Last Glacial Maximum: a data?model comparisonDoes plant size affect growth responses to water availability at glacial, modern and future CO2 concentrations?
P2860
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P2860
Climate change as the dominant control on glacial-interglacial variations in C3 and C4 plant abundance.
description
2001 nî lūn-bûn
@nan
2001 թուականի Օգոստոսին հրատարակուած գիտական յօդուած
@hyw
2001 թվականի օգոստոսին հրատարակված գիտական հոդված
@hy
2001年の論文
@ja
2001年論文
@yue
2001年論文
@zh-hant
2001年論文
@zh-hk
2001年論文
@zh-mo
2001年論文
@zh-tw
2001年论文
@wuu
name
Climate change as the dominant ...... in C3 and C4 plant abundance.
@ast
Climate change as the dominant ...... in C3 and C4 plant abundance.
@en
type
label
Climate change as the dominant ...... in C3 and C4 plant abundance.
@ast
Climate change as the dominant ...... in C3 and C4 plant abundance.
@en
prefLabel
Climate change as the dominant ...... in C3 and C4 plant abundance.
@ast
Climate change as the dominant ...... in C3 and C4 plant abundance.
@en
P2093
P356
P1433
P1476
Climate change as the dominant ...... in C3 and C4 plant abundance.
@en
P2093
Freeman KH
Metcalfe SE
Moreland M
Street-Perrott FA
P304
P356
10.1126/SCIENCE.1060143
P407
P577
2001-08-01T00:00:00Z