about
Constraining the role of early land plants in Palaeozoic weathering and global coolingEctomycorrhizal fungi and past high CO2 atmospheres enhance mineral weathering through increased below-ground carbon-energy fluxesEvolution of trees and mycorrhizal fungi intensifies silicate mineral weatheringBiological weathering and the long-term carbon cycle: integrating mycorrhizal evolution and function into the current paradigm.A Dynamic Hydro-Mechanical and Biochemical Model of Stomatal Conductance for C4 Photosynthesis.Increased susceptibility to drought-induced mortality in Sequoia sempervirens (Cupressaceae) trees under Cenozoic atmospheric carbon dioxide starvation.Enhanced weathering strategies for stabilizing climate and averting ocean acidificationWeathering by tree-root-associating fungi diminishes under simulated Cenozoic atmospheric CO<sub>2</sub> declineA glacier respires: Quantifying the distribution and respiration CO2flux of cryoconite across an entire Arctic supraglacial ecosystemInvestigating Devonian trees as geo-engineers of past climates: linking palaeosols to palaeobotany and experimental geobiologyC4 savanna grasses fail to maintain assimilation in drying soil under low CO2 compared with C3 trees despite lower leaf water demandStomatal and non-stomatal limitations in savanna trees and C4 grasses grown at low, ambient and high atmospheric CO2
P50
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P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Joe Quirk
@ast
Joe Quirk
@en
Joe Quirk
@es
Joe Quirk
@nl
type
label
Joe Quirk
@ast
Joe Quirk
@en
Joe Quirk
@es
Joe Quirk
@nl
prefLabel
Joe Quirk
@ast
Joe Quirk
@en
Joe Quirk
@es
Joe Quirk
@nl
P106
P1153
23670572400
P31
P496
0000-0002-0625-8323