2011
DOI: 10.1590/2175-7860201162210
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Floristics and life-forms along a topographic gradient, central-western Ceará, Brazil

Abstract: To test whether the flora is organized in discrete or continuous units along a topographic gradient, three physiognomies were assessed on different soil classes in a semi-arid region of northeastern Brazil: caatinga (xeric shrubland) at altitudes from 300 to 500 m, deciduous forest at altitudes from 500 to 700 m and carrasco (deciduous shrubland) at 700 m. In each physiognomy a species inventory was carried out, and plants were classified according to life- and growth-forms. Species richness was higher in the … Show more

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Cited by 47 publications
(51 citation statements)
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“…The study was carried out during nine nights in the dry season (July 2012) and 10 nights in the rainy season (February 2013) (ARAÚJO et al, 2011).…”
Section: Study Site and Capture Of Batsmentioning
confidence: 99%
“…The study was carried out during nine nights in the dry season (July 2012) and 10 nights in the rainy season (February 2013) (ARAÚJO et al, 2011).…”
Section: Study Site and Capture Of Batsmentioning
confidence: 99%
“…Both vegetation types grow in a semiarid climate and have different richness and abundance of lianas (Araújo & Martins 1999;Araújo et al 2011). The study areas are located within the Serra das Almas Private Natural Heritage Reserve (5°7'001"S and 40°52'220.79"W), which is in the mid-western region of the state of Ceará and is located in the northeastern semiarid region of Brazil.…”
Section: Study Area and Focal Speciesmentioning
confidence: 99%
“…Análises de padrões de diversidade, distribuição e endemismos das Leguminosae em áreas de caatingas com fisionomias aparentemente homogêneas têm demonstrado que, sob a denominação de caatinga, provavelmente existam duas biotas historicamente distintas (Queiroz 2006;Cardoso & Queiroz 2007). Estes autores argumentam que as ecorregiões da Caatinga poderiam ser subdivididas em uma biota associada às superfícies sedimentares arenosas, enquanto a outra associada aos solos geralmente pedregosos derivados de rochas cristalinas pré-cambrianas (Queiroz 2006;Cardoso & Queiroz 2007;Araújo et al 2011). De fato, além de apresentar maior densidade de indivíduos por espécie (AndradeLima 1981;Lyra 1982;Rodal 1992;Rocha et al 2004), a caatinga associada às bacias sedimentares é também mais rica em espécies e endemismos do que a caatinga sobre solos derivados do embasamento cristalino (Queiroz 2006).…”
Section: Introductionunclassified