Palaeoendemic plants provide evidence for persistence of open, well‐watered vegetation since the Cretaceous
AIM: Palaeoendemics are clades that are ancient but geographically restricted, often because they have been selected against in other areas. Ecological similarities among palaeoendemics may be indicators of ancient environments. We determine the environmental ranges of the remarkable palaeoendemic p...
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Published in | Global ecology and biogeography Vol. 25; no. 2; pp. 127 - 140 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Blackwell Science
01.02.2016
Blackwell Publishing Ltd John Wiley & Sons Ltd Wiley Subscription Services, Inc |
Subjects | |
Online Access | Get full text |
ISSN | 1466-822X 1466-8238 |
DOI | 10.1111/geb.12389 |
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Summary: | AIM: Palaeoendemics are clades that are ancient but geographically restricted, often because they have been selected against in other areas. Ecological similarities among palaeoendemics may be indicators of ancient environments. We determine the environmental ranges of the remarkable palaeoendemic plants of Tasmania to deduce whether they indicate the long‐term persistence of particular environmental conditions. LOCATION: Tasmania, Australia, a global centre of plant palaeoendemism, containing some of the world's most relictual plant lineages. METHODS: Palaeoendemic clades in Tasmania were identified using a scoring system of clade age divided by the square root of the number of 10 km × 10 km grid cells occupied globally. Total palaeoendemism scores for 1199 30″ grid cells were calculated by summing scores for individual clades, and modelled against climate, topography, geology and vegetation type using Random Forest models. Palaeoendemic and non‐palaeoendemic species richness in climate space was measured. The global distribution of climates favoured by palaeoendemics was assessed. RESULTS: Twenty‐nine phylogenetically and ecologically diverse palaeoendemic clades (51 species) were identified. High levels of palaeoendemism occurred widely in western Tasmania, but the highest scoring areas were at or slightly above the tree line in relatively undisturbed vegetation. Palaeoendemism scores were strongly predicted by constantly moist climates lacking extreme temperatures, and by open vegetation types with rare or no fire. The palaeoendemics occupied a climate space that is globally rare and very different from that of non‐palaeoendemics. MAIN CONCLUSIONS: These patterns suggest the persistence since the Cretaceous of open vegetation in constantly moist areas with equable temperatures and few or no fires. This conclusion is consistent with an increasing body of fossil and phylogenetic evidence for the antiquity of open vegetation. The methods here produce quantitative values of palaeoendemism that can be compared among regions. |
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Bibliography: | http://dx.doi.org/10.1111/geb.12389 istex:323C4CB3ED2F3AD6D3DF51DC25B2701E2E0865A4 ark:/67375/WNG-30PZBTV1-8 Figure S1 Observed palaeoendemism scores for the 1199 30″ grid cells under each of the alternative scoring scenarios. Table S1 Palaeoendemic clades in Tasmania. Table S2 Possibly palaeoendemic and nearly palaeoendemic clades not included in analyses. Table S3 Justification for the exclusion of Tasmanian clades as being unlikely to be palaeoendemic. Table S4 Translation of TASVEG vegetation types into the 12 vegetation types used in this study. Table S5 Major geological types used in this study. Table S6 Random Forest model output for each score class. Table S7 Variable importance measures for variables fitted with the various Random Forest models. ArticleID:GEB12389 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
ISSN: | 1466-822X 1466-8238 |
DOI: | 10.1111/geb.12389 |