2010
DOI: 10.1111/j.1466-8238.2010.00595.x
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Historical and phylogenetic constraints on the incidence of entire leaf margins: insights from a new South American model

Abstract: AimThe relationship between the proportion of species with an entire leaf margin (pE) and mean annual temperature (MAT) is one of the most powerful tools for estimating palaeotemperatures. However, phylogenetic and phytogeographic constraints on this relationship have remained unexplored. Here we investigate the pE-MAT relationship for modern floristic assemblages from southern South American forests, assess its conformity to other models and test for the existence of historical constraints on pE-MAT models. L… Show more

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Cited by 56 publications
(69 citation statements)
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References 50 publications
(101 reference statements)
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“…Towards the end of the Eocene, this Subtropical Gondwana Paleoflora of southern South America was replaced by Mixed Paleoflora, which in turn gave way to Subtropical Neogene Paleoflora indicating hot, humid conditions during the Early-Middle Miocene (Hinojosa andVillagrán, 1997, 2005). Maximum continental temperatures were reached between 17-15 Ma, as indicated by fossil leaves and pollen of Miocene deposits in Chile and Argentina (Hinojosa, 2005;Hinojosa et al, 2011). After the Middle Miocene Climatic Optimum, pollen records suggest a marked decrease in temperature attributed to glaciation in West Antarctica and the beginning of uplift in the Andes (Zachos et al, 2001).…”
Section: Continental Paleoclimatic Conditionsmentioning
confidence: 99%
See 1 more Smart Citation
“…Towards the end of the Eocene, this Subtropical Gondwana Paleoflora of southern South America was replaced by Mixed Paleoflora, which in turn gave way to Subtropical Neogene Paleoflora indicating hot, humid conditions during the Early-Middle Miocene (Hinojosa andVillagrán, 1997, 2005). Maximum continental temperatures were reached between 17-15 Ma, as indicated by fossil leaves and pollen of Miocene deposits in Chile and Argentina (Hinojosa, 2005;Hinojosa et al, 2011). After the Middle Miocene Climatic Optimum, pollen records suggest a marked decrease in temperature attributed to glaciation in West Antarctica and the beginning of uplift in the Andes (Zachos et al, 2001).…”
Section: Continental Paleoclimatic Conditionsmentioning
confidence: 99%
“…Belonging to the Subtropical Neogene Flora ('Pololos paleoflora' in figure 3), this suggests mean temperatures of 21-24ºC and a mean annual rainfall of 44-91 cm. There was thus a gradual increase in temperature and aridification between 16-12 Ma, which can be attributed to accelerated uplift in the Andes that prevented the spill-over of humid air from the east Hinojosa et al, 2011). Finally, pollen with affinity to modern Araucaria angustifolia (Bertol) and Araucaria araucana (Koch) occur together in both the lower and upper units, but these species are presently separated by the Arid Diagonal.…”
Section: Continental Paleoclimatic Conditionsmentioning
confidence: 99%
“…A Eq. 5 é a mais precisa para o calculo da temperatura (Tabela 4, Figura 7), como também fora comprovado por outros autores (Hinojosa et al 2011;Fanton, 2013) que as aplicaram para florestas tropicais e austrais da América do Sul. Os conjuntos de amostras provenientes dos diques marginais de rio e associadas ao Cerrado na área estudada refletem melhor a temperatura quando utilizadas as equações baseadas no LMA.…”
Section: Análises Climáticas Da Morfologia Das Folhasunclassified
“…Степень изрезанности края листа ископаемых растений широко используется для реконструкции континентальных палеотемператур (Wolfe, 1971;Dolph, 1979;Wolfe, 1993;Wilf, 1997;Royer, Wilf, 2006;Adams et al, 2008;Royer et al, 2009;Hinojosa et al, 2011;Royer et al, 2012).…”
Section: Introductionunclassified