Large inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum

Large inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum is …
instance of (P31):
scholarly articleQ13442814

External links are
P356DOI10.1038/NGEO1324

P50authorCharles KovenQ57299102
Philippe CiaisQ33142437
Alessandro TagliabueQ44677031
Iain Colin PrenticeQ55190913
Laurent BoppQ56462055
P2093author name stringG. Hoffmann
A. Lourantou
M. Cuntz
S. P. Harrison
M. Scholze
S. L. Piao
D. I. Kelley
P2860cites workMid-Holocene and glacial-maximum vegetation geography of the northern continents and AfricaQ57264474
The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannasQ57264661
The climate induced variation of the continental biosphere: A model simulation of the Last Glacial MaximumQ57950312
Carbon-biosphere-climate interactions in the last glacial maximum climateQ57950342
Constraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciationQ58087586
Simulating changes in the terrestrial biosphere during the last glacial/interglacial transitionQ58087634
Evaluation of the terrestrial carbon cycle, future plant geography and climate-carbon cycle feedbacks using five Dynamic Global Vegetation Models (DGVMs)Q58267207
Climate change and Arctic ecosystems: 1. Vegetation changes north of 55°N between the last glacial maximum, mid-Holocene, and presentQ58397091
Biospheric carbon stocks reconstructed at the Last Glacial Maximum: comparison between general circulation models using prescribed and computed sea surface temperaturesQ58647147
Terrestrial carbon storage at the LGMQ59061829
The sensitivity of terrestrial carbon storage to climate changeQ59096858
Terrestrial carbon-storage from the last glacial maximum to the presentQ60545656
The Dole Effect and its variations during the last 130,000 years as measured in the Vostok Ice CoreQ63777274
Influence of carbonic anhydrase activity in terrestrial vegetation on the 18O content of atmospheric CO2Q73703508
High-precision measurements of 17O/16O and 18O/16O of O2 and O2/Ar ratio in airQ79364935
Extensive Methane Venting to the Atmosphere from Sediments of the East Siberian Arctic ShelfQ24289129
A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP)Q29028344
Increases in terrestrial carbon storage from the Last Glacial Maximum to the presentQ29304697
Climate change. Permafrost and the global carbon budgetQ31044392
Terrestrial gross carbon dioxide uptake: global distribution and covariation with climateQ34124447
Global vegetation and terrestrial carbon cycle changes after the last ice age.Q39368085
Role of marine biology in glacial-interglacial CO2 cyclesQ47303317
Ice Age terrestrial carbon changes revisitedQ55888637
Soil organic carbon pools in the northern circumpolar permafrost regionQ55894469
THE RELATIVE ATOMIC WEIGHT OF OXYGEN IN WATER AND IN AIRQ55980293
Carbon stocks and isotopic budgets of the terrestrial biosphere at mid-Holocene and last glacial maximum timesQ56100477
Lowering of glacial atmospheric CO2in response to changes in oceanic circulation and marine biogeochemistryQ56554727
Biological oxygen productivity during the last 60,000 years from triple oxygen isotope measurementsQ56835170
Dust impact on marine biota and atmospheric CO2during glacial periodsQ57038357
A model of the Earth's Dole effectQ57242267
A three-dimensional synthesis study of δ18O in atmospheric CO2: 1. Surface fluxesQ57242389
Modeling fire and the terrestrial carbon balanceQ57264370
The influence of vegetation, fire spread and fire behaviour on biomass burning and trace gas emissions: results from a process-based modelQ57264384
Pollen-based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0, 6000 and 18,000 14C yr BPQ57264431
Climate and CO2 controls on global vegetation distribution at the last glacial maximum: analysis based on palaeovegetation data, biome modelling and palaeoclimate simulationsQ57264440
P433issue1
P407language of work or nameEnglishQ1860
P921main subjectlast glacial maximumQ1979625
biosphereQ42762
P304page(s)74-79
P577publication date2011-11-20
P1433published inNature GeoscienceQ1337483
P1476titleLarge inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum
P478volume5

Reverse relations

cites work (P2860)
Q5789044820th century changes in carbon isotopes and water-use efficiency: tree-ring-based evaluation of the CLM4.5 and LPX-Bern models
Q58054865A lower limit to atmospheric CO2 concentrations over the past 800,000 years
Q34213620Carbon isotope constraints on the deglacial CO₂ rise from ice cores
Q57070771Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost
Q30962841Effects of fire and CO2 on biogeography and primary production in glacial and modern climates
Q94474068Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
Q59095940Extensive loss of past permafrost carbon but a net accumulation into present-day soils
Q31049820Global pulses of organic carbon burial in deep-sea sediments during glacial maxima
Q58317970Higher climatological temperature sensitivity of soil carbon in cold than warm climates
Q57160835Historical carbon dioxide emissions caused by land-use changes are possibly larger than assumed
Q58072132Influence of dynamic vegetation on climate change and terrestrial carbon storage in the Last Glacial Maximum
Q28658467Larger CO₂ source at the equatorial Pacific during the last deglaciation
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Q94592051Millennial-scale hydroclimate control of tropical soil carbon storage
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Q42006825Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød
Q57900985Perspectives on the Terrestrial Organic Matter Transport and Burial along the Land-Deep Sea Continuum: Caveats in Our Understanding of Biogeochemical Processes and Future Needs
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Q40835434Responses of ocean circulation and carbon cycle to changes in the position of the Southern Hemisphere westerlies at Last Glacial Maximum
Q97533950Self-sustained oscillations and global climate changes
Q57196310Simulating soil organic carbon in yedoma deposits during the Last Glacial Maximum in a land surface model
Q28645614The deep permafrost carbon pool of the Yedoma region in Siberia and Alaska
Q58396934What have we learnt from palaeoclimate simulations?

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