<HashMap><database>biostudies-literature</database><scores><citationCount>0</citationCount><reanalysisCount>0</reanalysisCount><viewCount>46</viewCount><searchCount>0</searchCount></scores><additional><omics_type>Unknown</omics_type><volume>105(3)</volume><submitter>Haworth M</submitter><pubmed_abstract>&lt;h4>Background and aims&lt;/h4>The inverse relationship between stomatal density (SD: number of stomata per mm(2) leaf area) and atmospheric concentration of CO2 ([CO2]) permits the use of plants as proxies of palaeo-atmospheric CO2. Many stomatal reconstructions of palaeo-[CO2] are based upon multiple fossil species. However, it is unclear how plants respond to [CO2] across genus, family or ecotype in terms of SD or stomatal index (SI: ratio of stomata to epidermal cells). This study analysed the stomatal numbers of conifers from the ancient family Cupressaceae, in order to examine the nature of the SI-[CO2] relationship, and potential implications for stomatal reconstructions of palaeo-[CO2]. Methods Stomatal frequency measurements were taken from historical herbarium specimens of Athrotaxis cupressoides, Tetraclinis articulata and four Callitris species, and live A. cupressoides grown under CO2-enrichment (370, 470, 570 and 670 p.p.m. CO2).&lt;h4>Key results&lt;/h4>T. articulata, C. columnaris and C. rhomboidea displayed significant reductions in SI with rising [CO2]; by contrast, A. cupressoides, C. preissii and C. oblonga show no response in SI. However, A. cupressoides does reduce SI to increases in [CO2] above current ambient (approx. 380 p.p.m. CO2). This dataset suggests that a shared consistent SI-[CO2] relationship is not apparent across the genus Callitris. Conclusions The present findings suggest that it is not possible to generalize how conifer species respond to fluctuations in [CO2] based upon taxonomic relatedness or habitat. This apparent lack of a consistent response, in conjunction with high variability in SI, indicates that reconstructions of absolute palaeo-[CO2] based at the genus level, or upon multiple species for discrete intervals of time are not as reliable as those based on a single or multiple temporally overlapping species.</pubmed_abstract><journal>Annals of botany</journal><pagination>411-8</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC2826259</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Differences in the response sensitivity of stomatal index to atmospheric CO2 among four genera of Cupressaceae conifers.</pubmed_title><pmcid>PMC2826259</pmcid><pubmed_authors>Heath J</pubmed_authors><pubmed_authors>McElwain JC</pubmed_authors><pubmed_authors>Haworth M</pubmed_authors><view_count>46</view_count></additional><is_claimable>false</is_claimable><name>Differences in the response sensitivity of stomatal index to atmospheric CO2 among four genera of Cupressaceae conifers.</name><description>&lt;h4>Background and aims&lt;/h4>The inverse relationship between stomatal density (SD: number of stomata per mm(2) leaf area) and atmospheric concentration of CO2 ([CO2]) permits the use of plants as proxies of palaeo-atmospheric CO2. Many stomatal reconstructions of palaeo-[CO2] are based upon multiple fossil species. However, it is unclear how plants respond to [CO2] across genus, family or ecotype in terms of SD or stomatal index (SI: ratio of stomata to epidermal cells). This study analysed the stomatal numbers of conifers from the ancient family Cupressaceae, in order to examine the nature of the SI-[CO2] relationship, and potential implications for stomatal reconstructions of palaeo-[CO2]. Methods Stomatal frequency measurements were taken from historical herbarium specimens of Athrotaxis cupressoides, Tetraclinis articulata and four Callitris species, and live A. cupressoides grown under CO2-enrichment (370, 470, 570 and 670 p.p.m. CO2).&lt;h4>Key results&lt;/h4>T. articulata, C. columnaris and C. rhomboidea displayed significant reductions in SI with rising [CO2]; by contrast, A. cupressoides, C. preissii and C. oblonga show no response in SI. However, A. cupressoides does reduce SI to increases in [CO2] above current ambient (approx. 380 p.p.m. CO2). This dataset suggests that a shared consistent SI-[CO2] relationship is not apparent across the genus Callitris. Conclusions The present findings suggest that it is not possible to generalize how conifer species respond to fluctuations in [CO2] based upon taxonomic relatedness or habitat. This apparent lack of a consistent response, in conjunction with high variability in SI, indicates that reconstructions of absolute palaeo-[CO2] based at the genus level, or upon multiple species for discrete intervals of time are not as reliable as those based on a single or multiple temporally overlapping species.</description><dates><release>2010-01-01T00:00:00Z</release><publication>2010 Mar</publication><modification>2024-11-10T02:49:15.19Z</modification><creation>2019-03-26T22:31:56Z</creation></dates><accession>S-EPMC2826259</accession><cross_references><pubmed>20089556</pubmed><doi>10.1093/aob/mcp309</doi></cross_references></HashMap>