2012
DOI: 10.1098/rstb.2011.0248
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Evolutionary context for understanding and manipulating plant responses to past, present and future atmospheric [CO 2 ]

Abstract: Variation in atmospheric [CO 2 ] is a prominent feature of the environmental history over which vascular plants have evolved. Periods of falling and low [CO 2 ] in the palaeo-record appear to have created selective pressure for important adaptations in modern plants. Today, rising [CO 2 ] is a key component of anthropogenic global environmental change that will impact plants and the ecosystem goods and services they deliver. Currently, there is limited evidence that natural plant populations have evolved in… Show more

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Cited by 79 publications
(83 citation statements)
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References 147 publications
(208 reference statements)
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“…Our hypothesis adds the evolution of C 4 photosynthesis to the list of exceptional innovations based on the plant hydraulic system that arose during periods of low CO 2 that have impacted on plant life history, biogeography and the distribution of ecosystems in the deep past, present and future [107]. Previously hypothesized modifications of the water transport system and associated plant features driven by low CO 2 include the evolution of xylem vessels and stomata [108], and the planate leaf [109,110] with high vein density [78].…”
Section: Resultsmentioning
confidence: 99%
“…Our hypothesis adds the evolution of C 4 photosynthesis to the list of exceptional innovations based on the plant hydraulic system that arose during periods of low CO 2 that have impacted on plant life history, biogeography and the distribution of ecosystems in the deep past, present and future [107]. Previously hypothesized modifications of the water transport system and associated plant features driven by low CO 2 include the evolution of xylem vessels and stomata [108], and the planate leaf [109,110] with high vein density [78].…”
Section: Resultsmentioning
confidence: 99%
“…We may be able to draw from the paleoecological literature to understand extinction risks, migration rates, and potential adaptive responses to climate change (Davis and Shaw, 2001;Leakey and Lau, 2012), especially by focusing on the few geological intervals during which the rate and magnitude of naturally induced climate change were similar to contemporary climate change driven by anthropogenic processes (Willis and MacDonald, 2011). During four geological periods of rapid climate change, macrofossil and pollen records document extensive changes in species' distribution patterns, but species likely also adapted to novel climates (for review, see Willis and MacDonald, 2011).…”
Section: Responses To Climate Change In Contemporary Versus Paleocommmentioning
confidence: 99%
“…Manipulative experiments that include replicated genotypes of known origin, collected from multiple populations across the range of a species, can test all of the hypotheses in Table I (Leakey and Lau, 2012), especially when combined with provenance trials or longitudinal studies. Comparisons of ancestral (pretreatment) and descendant (posttreatment) genotypes in artificial selection experiments can also be used to evaluate whether adaptation to climate change is likely, and if so, how many generations will be needed (Kelly et al, 2012).…”
Section: Simulate Predisturbance and Postdisturbance Conditions Expermentioning
confidence: 99%
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