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Registro Completo |
Biblioteca(s): |
Embrapa Pantanal. |
Data corrente: |
04/02/2011 |
Data da última atualização: |
15/02/2013 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
OLIFIERS, N.; BIANCHI, R. de C.; D'ANDREA, P. S.; MOURAO, G. de M.; GOMPPER, M. E. |
Afiliação: |
NATALIE OLIFIERS, UNIVERSITY OF MISSOURI; RITA DE CÁSSIA BIANCHI, UFMS; PAULO SÉRGIO D'ANDREA, INSTITUTO OSWALDO CRUZ; GUILHERME DE MIRANDA MOURAO, CPAP; MATTHEW E. GOMPPER, UNIVERSITY OF MISSOURI. |
Título: |
Estimating age of carnivores from the Pantanal region of Brazil. |
Ano de publicação: |
2010 |
Fonte/Imprenta: |
Wildlife Biology, v. 16, n. 4, p. 389-399, 2010. |
Idioma: |
Inglês |
Conteúdo: |
Conservation and management of animal populations often require knowledge about the age structure, but this information is usually difficult to discern. We propose a method to estimate the age of carnivores based on dental condition and body size measurements, and we apply the method to populations of brown-nosed coatis Nasua nasua and crab-eating foxes Cerdocyon thous in the Brasilian Pantanal. |
Palavras-Chave: |
Brown-nosed coati; Crab-eating fox; Dental condition. |
Thesaurus Nal: |
age; body size; Cerdocyon thous; Nasua nasua; Pantanal. |
Categoria do assunto: |
-- |
Marc: |
LEADER 01094naa a2200265 a 4500 001 1875824 005 2013-02-15 008 2010 bl --- 0-- u #d 100 1 $aOLIFIERS, N. 245 $aEstimating age of carnivores from the Pantanal region of Brazil. 260 $c2010 520 $aConservation and management of animal populations often require knowledge about the age structure, but this information is usually difficult to discern. We propose a method to estimate the age of carnivores based on dental condition and body size measurements, and we apply the method to populations of brown-nosed coatis Nasua nasua and crab-eating foxes Cerdocyon thous in the Brasilian Pantanal. 650 $aage 650 $abody size 650 $aCerdocyon thous 650 $aNasua nasua 650 $aPantanal 653 $aBrown-nosed coati 653 $aCrab-eating fox 653 $aDental condition 700 1 $aBIANCHI, R. de C. 700 1 $aD'ANDREA, P. S. 700 1 $aMOURAO, G. de M. 700 1 $aGOMPPER, M. E. 773 $tWildlife Biology$gv. 16, n. 4, p. 389-399, 2010.
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Embrapa Pantanal (CPAP) |
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Registro Completo
Biblioteca(s): |
Embrapa Meio Ambiente. |
Data corrente: |
09/12/2019 |
Data da última atualização: |
09/12/2019 |
Tipo da produção científica: |
Resumo em Anais de Congresso |
Autoria: |
GREEN, T. R.; ERSKINE, R. H.; KIPKA, H.; LIGHTHART, N.; EDMUNDS, D. A.; McMASTER, G. S.; DAVID, O.; CRUZ, P. P. N. da; FIGUEIREDO, R. de O. |
Afiliação: |
T. R. GREEN, USDA - United States Department of Agriculture, Colorado State University (CSU); R. H. ERSKINE; H. KIPKA; N. LIGHTHART; D. A. EDMUNDS; G. S. McMASTER; O. DAVID; PATRÍCIA PORTA NOVA DA CRUZ, Programa CSF do CNPq.; RICARDO DE OLIVEIRA FIGUEIREDO, CNPMA. |
Título: |
Integration of distributed measurements and simulations to explore spatial complexity in a field-scale agricultural watershed. |
Ano de publicação: |
2019 |
Fonte/Imprenta: |
In: Soil Science Society of America International Soils Meeting, 2019, San Diego, California. Soils Across Latitudes: [abstracts...] San Diego: SSSA, 2019. Ref. 44-2. |
Idioma: |
Inglês |
Conteúdo: |
Long-term measurements of high-resolution soil moisture across rolling terrain facilitate complex simulations of surface hydrology and soil moisture dynamics. Soil hydraulic properties that control water storage flow rates can vary markedly in space, and surface layers may vary temporally due to management events, reconsolidation and biological activity. Field measurements are expensive to collect and generally reveal complex variability that is difficult to fully characterize. Yet, these soil properties are represented using model parameters that may strongly affect simulated flows and the distribution of soil water in space and time. Thus model calibration using available measurements of soil moisture and surface runoff is essential. Here, we address the model spatial resolution and calibration detail needed to estimate available data by using five levels of spatial complexity from homogeneous to fully three-dimensional calibrated soil parameters. Issues of spatial scaling are also explored. Furthermore, a new model component of temporal changes in soil porosity and saturated hydraulic conductivity is tested to simulate effects of tillage and soil consolidation related to rainfall. Interactions between spatial and temporal parameters and processes will be discussed in terms of their influences on simulated soil moisture patterns and surface runoff. |
Thesagro: |
Bacia Hidrográfica; Hidrologia; Solo. |
Thesaurus NAL: |
Soil; Watersheds. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/206494/1/RA-FigueiredoRO-SSSAInternationalSoilsMeeting-2019.pdf
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Marc: |
LEADER 02274nam a2200265 a 4500 001 2116366 005 2019-12-09 008 2019 bl uuuu u00u1 u #d 100 1 $aGREEN, T. R. 245 $aIntegration of distributed measurements and simulations to explore spatial complexity in a field-scale agricultural watershed.$h[electronic resource] 260 $aIn: Soil Science Society of America International Soils Meeting, 2019, San Diego, California. Soils Across Latitudes: [abstracts...] San Diego: SSSA, 2019. Ref. 44-2.$c2019 520 $aLong-term measurements of high-resolution soil moisture across rolling terrain facilitate complex simulations of surface hydrology and soil moisture dynamics. Soil hydraulic properties that control water storage flow rates can vary markedly in space, and surface layers may vary temporally due to management events, reconsolidation and biological activity. Field measurements are expensive to collect and generally reveal complex variability that is difficult to fully characterize. Yet, these soil properties are represented using model parameters that may strongly affect simulated flows and the distribution of soil water in space and time. Thus model calibration using available measurements of soil moisture and surface runoff is essential. Here, we address the model spatial resolution and calibration detail needed to estimate available data by using five levels of spatial complexity from homogeneous to fully three-dimensional calibrated soil parameters. Issues of spatial scaling are also explored. Furthermore, a new model component of temporal changes in soil porosity and saturated hydraulic conductivity is tested to simulate effects of tillage and soil consolidation related to rainfall. Interactions between spatial and temporal parameters and processes will be discussed in terms of their influences on simulated soil moisture patterns and surface runoff. 650 $aSoil 650 $aWatersheds 650 $aBacia Hidrográfica 650 $aHidrologia 650 $aSolo 700 1 $aERSKINE, R. H. 700 1 $aKIPKA, H. 700 1 $aLIGHTHART, N. 700 1 $aEDMUNDS, D. A. 700 1 $aMcMASTER, G. S. 700 1 $aDAVID, O. 700 1 $aCRUZ, P. P. N. da 700 1 $aFIGUEIREDO, R. de O.
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