scholarly journals Atmospheric carbon dioxide: a driver of photosynthetic eukaryote evolution for over a billion years?

2012 ◽  
Vol 367 (1588) ◽  
pp. 477-482 ◽  
Author(s):  
David J. Beerling

Exciting evidence from diverse fields, including physiology, evolutionary biology, palaeontology, geosciences and molecular genetics, is providing an increasingly secure basis for robustly formulating and evaluating hypotheses concerning the role of atmospheric carbon dioxide (CO 2 ) in the evolution of photosynthetic eukaryotes. Such studies span over a billion years of evolutionary change, from the origins of eukaryotic algae through to the evolution of our present-day terrestrial floras, and have relevance for plant and ecosystem responses to future global CO 2 increases. The papers in this issue reflect the breadth and depth of approaches being adopted to address this issue. They reveal new discoveries pointing to deep evidence for the role of CO 2 in shaping evolutionary changes in plants and ecosystems, and establish an exciting cross-disciplinary research agenda for uncovering new insights into feedbacks between biology and the Earth system.

BioScience ◽  
2004 ◽  
Vol 54 (8) ◽  
pp. 731 ◽  
Author(s):  
YIQI LUO ◽  
BO SU ◽  
WILLIAM S. CURRIE ◽  
JEFFREY S. DUKES ◽  
ADRIEN FINZI ◽  
...  

2016 ◽  
Vol 27 (6-7) ◽  
pp. 785-797 ◽  
Author(s):  
Martin Hertzberg ◽  
Hans Schreuder

1998 ◽  
Vol 1 (1) ◽  
pp. 27-38 ◽  
Author(s):  
Stephen Wiel ◽  
Nathan Martin ◽  
Mark Levine ◽  
Lynn Price ◽  
Jayant Sathaye

Knowledge about the effects of the rise in atmospheric CO 2 concentration on trees and forest is assessed and, the converse, the possible impact of forests on the atmospheric CO 2 concentration is discussed. At the cellular scale, much is known about the role of CO 2 as a substrate in photosynthesis, but only little about its role as an activator and regulator. At the leaf scale, the response of CO 2 assimilation to CO 2 concentration has been described often and is well represented by biochemically based models, but there is inadequate information to parametrize the models of CO 2 -acclimated leaves. Growth and partitioning to the roots of seedlings and young trees generally increases in response to a doubling in atmospheric CO 2 concentration. Experimental results are very variable, because of the differing length of the experiments, the artificial conditions and the artefactual constraints. At larger scales, direct measurements of responses to increase in atmospheric CO 2 are impractical but models of canopy processes suggest that significant increases in CO 2 assimilation will result from the rise in atmospheric concentration. Inferences from the increase in amplitude of the seasonal oscillation in the global atmospheric CO 2 concentration at different latitudes suggest that forest is having a significant impact on the global atmospheric concentration, but it seems unlikely that expansion of the forest resource could effectively reduce the increase in atmospheric CO 2 .


2017 ◽  
Author(s):  
Eko Haryono

The important of karst denudation in term of climate changes lies on the ability of karst ecosystem inregulating atmospheric carbon. Karst denudation consumes CO2 either from atmosphere and soils. Thispaper is intended to describe the karst denudation related to CO2 sequestration and apply the concept tocalculate carbon gain through karst denudation process in Indonesian. Estimated from the carbonate rockoutcrops, the Indonesian karst region is approximately 140,000,000 km2. Previous work suggested thataverage denudation rate of Indonesian karst is 82.9 m3/year/km2 or equivalent to 218,856 kg/year/km2.Since 120 kg of atmospheric carbon is absorbed during the removal of one ton calcium carbonate removaland Indonesia karst area is 140.000 km2, Indonesian karst area up takes 3,677 Gg/year atmosphericcarbon. This amount is equivalent to 13.482 Gg CO2/year. This figure is merely from denudationprocesses, considering carbon dioxide sequestration by karst vegetation covers will inevitably gains muchhigher number. The role of karst denudation therefore needs more attention in carbon flux calculation anddeveloping climate change mitigation measures


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