A Herpetofauna Do Parque Nacional Da Serra Das Confusões, Piauí, Brasil, Com Uma Lista Regional Para Uma área Ecotonal Entre O Cerrado E A Caatinga

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Different physiognomies at Parque Nacional da Serra das Confusões (PNSCo) were intensively sampled aiming to access the distribution pattern of its herpetofauna. Sixty six species were found in the park (47 reptiles and 19 amphibians); the rarefaction curve for lizards, although not fully stabilized in an asymptote, indicates that the sampling effort was enough to reveal most lizard species occurring in the area; and richness estimators recovered values close to observed. For amphibians, the curve shows a weak tendency to stabilization with richness estimators indicating that additional records could be done. Field work carried out at PNSCo has highlighted an unique herpetofauna: five new species were described and there are three candidates as new species. The regional list including Cerrados’s units - Estação Ecológica Serra Geral do Tocantins (EESGT) and Estação Ecológica de Uruçuí-Una (EEUU) with Caatinga’s ones - PNSCo and Parque Nacional da Serra da Capivara (PNSCa), shows a high herpetofaunal diversity (191 species) to the region. The cluster analysis recovered the Cerrados’s units and Caatinga’s ones, in separate clusters evidencing a species turnover between domains, despite its geographical proximity. Thus, although there is widespread fauna throughout region shared by the units, each reserve holds its own faunal identity, harboring a singular assemblage of species. © 2016, Universidade Estadual de Campinas UNICAMP. All rights reserved.1632011/50206-9, FAPESP, Fundação de Amparo Pesquisa do Estado de São Paulo303545/2010-0, CNPq, Conselho Nacional de Desenvolvimento Científico e Tecnológico565046/2010-1, CNPq, Conselho Nacional de Desenvolvimento Científico e TecnológicoFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq

Análise de crescimento e anatomia foliar da planta medicinal Ageratum conyzoides L. (Asteraceae) cultivada em diferentes substratos

Ageratum conyzoides L. (Asteraceae) é uma espécie herbácea que ocorre em áreas de cerrado e, por se tratar de planta medicinal, é cultivada em escala familiar. O objetivo deste trabalho foi estudar possíveis alterações no desenvolvimento das plantas quando cultivadas em solos com texturas diferentes (solo de cerrado, franco arenoso ou solo de terra roxa, muito argiloso). Foram analisados aos 40, 70 e 90 dias, o comprimento do caule e da raiz, massa seca da parte aérea (caule e folhas) e das raízes, número de folhas e área foliar; além de parâmetros anatômicos foliares, como a densidade de tricomas. Os resultados mostraram que os comprimentos do caule e da raiz aumentaram no decorrer do experimento, independentemente do substrato (com exceção do comprimento da raiz de plantas cultivadas em solo de terra roxa). Porém, o comprimento do caule foi sempre maior nas plantas cultivadas em solo de cerrado, enquanto o comprimento da raiz foi significativamente maior somente aos 90 dias de cultivo neste solo. As biomassas secas da raiz e do caule também foram maiores nas plantas cultivadas em solo de cerrado por 70 e 90 dias, respectivamente. A massa seca foliar foi maior nas plantas cultivadas em solo de cerrado a partir dos 70 dias de experimento. Esse aumento foi devido ao maior número de folhas produzidas e a maior área foliar dessas plantas. No geral, a anatomia foliar não diferiu, porém o número de tricomas glandulares foi maior nas plantas cultivadas em solo de cerrado. Os resultados indicaram que esta espécie tem melhor desenvolvimento quando cultivada em solo mais arenoso.Ageratum conyzoides L. (Asteraceae) is a herbaceous species found in cerrado areas and grown in family scale since it is a medicinal plant. The aim of this work was to study possible alterations in the plant development when grown in soils presenting different textures (a sandy-loam cerrado soil, or a very clayish red earth soil). At 40, 70 and 90 days, stem and root length, shoot (stem and leaves) and root dry matter, number of leaves and leaf area were evaluated, in addition to leaf anatomical parameters, such as trichome density. Stem and root length increased over the experiment under any substrate (except root length of plants grown on red earth soil). However, stem length was always higher in plants grown on cerrado soil, whereas root length was significantly higher only at 90 days of cultivation on this same soil. Root and stem dry biomass were also higher in plants grown on cerrado soil at 70 and 90 days, respectively. Leaf dry matter was higher in plants grown on cerrado soil from 70 days of experiment. This increase was due to the larger number of produced leaves and the higher leaf area of those plants. In general, leaf anatomy does not differ; however, the number of glandular trichomes was larger in plants grown on cerrado soil. Such results indicated that this species had a better development when grown on sandier soils

Beyond Refugia: New insights on Quaternary climate variation and the evolution of biotic diversity in tropical South America

Haffer’s (Science 165: 131–137, 1969) Pleistocene refuge theory has provided motivation for 50 years of investigation into the connections between climate, biome dynamics, and neotropical speciation, although aspects of the orig- inal theory are not supported by subsequent studies. Recent advances in paleocli- matology suggest the need for reevaluating the role of Quaternary climate on evolutionary history in tropical South America. In addition to the many repeated large-amplitude climate changes associated with Pleistocene glacial-interglacial stages (~40 kyr and 100 kyr cyclicity), we highlight two aspects of Quaternary climate change in tropical South America: (1) an east-west precipitation dipole, induced by solar radiation changes associated with Earth’s precessional variations (~20 kyr cyclicity); and (2) periods of anomalously high precipitation that persisted for centuries-to-millennia (return frequencies ~1500 years) congruent with cold “Heinrich events” and cold Dansgaard-Oeschger “stadials” of the North Atlantic region. The spatial footprint of precipitation increase due to this North Atlantic forcing extended across almost all of tropical South America south of the equator. Combined, these three climate modes present a picture of climate change with different spatial and temporal patterns than envisioned in the original Pleistocene refuge theory. Responding to these climate changes, biomes expanded and contracted and became respectively connected and disjunct. Biome change undoubtedly influenced biotic diversification, but the nature of diversification likely was more complex than envisioned by the original Pleistocene refuge theory. In the lowlands, intermittent forest expansion and contraction led to species dispersal and subsequent isolation, promoting lineage diversification. These pulses of climate-driven biotic interchange profoundly altered the composition of regional species pools and triggered new evolutionary radiations. In the special case of the tropical Andean forests adjacent to the Amazon lowlands, new phylogenetic data provide abundant evidence for rapid biotic diversification during the Pleistocene. During warm interglacials and intersta- dials, lowland taxa dispersed upslope. Isolation in these disjunct climate refugia led to extinction for some taxa and speciation for others.Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/155561/1/Baker2020.pdfDescription of Baker2020.pdf : Main articl

Effect of coupling excess pore pressure and soil deformation on nonlinear SSI in liquefiable soil deposits

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