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Registro Completo |
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Biblioteca(s): |
Embrapa Agrossilvipastoril. |
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Data corrente: |
14/01/2015 |
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Data da última atualização: |
14/01/2015 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
CORDEIRO, R. C.; TURCQ, B.; MOREIRA, L. S.; RODRIGUES, R. de A. R.; SIMÕES FILHO, F. F. L.; MARTINS, G. S.; SANTOS, A. B.; BARBOSA, M.; CONCEIÇÃO, M. C. G. da; RODRIGUES, R. de C.; EVANGELISTA, H.; MOREIRA-TURCQ, P.; PENIDO, Y. P.; SIFEDDINE, A.; SEOANE, J. C. S. |
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Afiliação: |
RENATO CAMPELLO CORDEIRO, UFF; BRUNO TURCQ, IRD-LOCEAN; LUCIANE SILVA MOREIRA, UFF; RENATO DE ARAGAO RIBEIRO RODRIGUES, CPAMT; FRANCISCO FERNANDO LAMEGO SIMÕES FILHO, IEN; GABRIEL SOUZA MARTINS, UFF; ALICE BOSCO SANTOS, UFF; MARCELO BARBOSA, UFRJ; MARCELA CARDOSO GUILLES DA CONCEIÇÃO, UFF; RODRIGO DE CARVALHO RODRIGUES, UFF; HEITOR EVANGELISTA, UERJ-LARAMG; PATRICIA MOREIRA-TURCQ, IRD-GET; YVAGA POTY PENIDO, UFF; ABDELFETTAH SIFEDDINE, UFF; JOSÉ CARLOS SÍCOLI SEOANE, UFRJ. |
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Título: |
Palaeofires in Amazon: Interplay between land use change and palaeoclimatic events |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Palaeogeography, Palaeoclimatology, Palaeoecology, v. 415, p.137-151, dez. 2014 |
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Páginas: |
15 |
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ISSN: |
0031-0182 |
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DOI: |
http://dx.doi.org.ez103.periodicos.capes.gov.br/10.1016/j.palaeo.2014.07.020 |
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Idioma: |
Inglês |
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Conteúdo: |
Interpreting the geological record of Amazon biomass combustion requires comparing charcoal accumulation rates in various biomes at different time scales. Charcoal accumulation rates, a proxy for palaeofire records, were obtained in sediment cores from Amazon lakes surrounded by several vegetation types and from a reservoirs in an intense land use change region. The records presented in this study were obtained in the following areas i) a reservoirs in Alta Floresta region (northern Mato Grosso State); ii) Lago do Saci (southern Pará State), a lake close to Alta Floresta and located at the southern border of Pará State; iii) a bog in an ecotone area in the Humaitá region (southern Amazonas State); iv) lakes in lateritic iron crust of the Carajás Hills (southeastern Pará State); v) Lago Comprido, a floodplain lake close to the Amazon River and surrounded by tropical rain forest (Monte Alegre, Pará State; vi) Lagoa da Pata in the Morro dos Seis Lagos alkaline complex (São Gabriel da Cachoeira, Amazonas State) and vii) Lago Caracaranã, a secluded lake in the northern Amazon cerrado (Roraima State). The highest charcoal accumulation rates were observed for modern records related to an intense change in land use at Alta Floresta, which had no precedent during the Holocene history of the Amazon. High charcoal accumulation rates that were observed in the Carajás region during low lake level phases in the Amazon in the mid-Holocene were comparable to those at the onset of the human settlement in Alta Floresta region. An increase in charcoal accumulation rate was observed in the late Holocene when the lake level was high, suggesting an interaction between climates and human presence. Low charcoal accumulation rates are typical of modern high rainfall environments, as observed in Lagoa da Pata where the environment is not susceptible to occurrences of wildfires even during relatively drier climatic phases. Low charcoal accumulation rates also exist in the relatively dry cerrado (savanna type) biome even during relatively dry phases in the Caracaranã region where the savanna-type vegetation biomass is lower and thus generates less charcoal particles than forest ecosystems. MenosInterpreting the geological record of Amazon biomass combustion requires comparing charcoal accumulation rates in various biomes at different time scales. Charcoal accumulation rates, a proxy for palaeofire records, were obtained in sediment cores from Amazon lakes surrounded by several vegetation types and from a reservoirs in an intense land use change region. The records presented in this study were obtained in the following areas i) a reservoirs in Alta Floresta region (northern Mato Grosso State); ii) Lago do Saci (southern Pará State), a lake close to Alta Floresta and located at the southern border of Pará State; iii) a bog in an ecotone area in the Humaitá region (southern Amazonas State); iv) lakes in lateritic iron crust of the Carajás Hills (southeastern Pará State); v) Lago Comprido, a floodplain lake close to the Amazon River and surrounded by tropical rain forest (Monte Alegre, Pará State; vi) Lagoa da Pata in the Morro dos Seis Lagos alkaline complex (São Gabriel da Cachoeira, Amazonas State) and vii) Lago Caracaranã, a secluded lake in the northern Amazon cerrado (Roraima State). The highest charcoal accumulation rates were observed for modern records related to an intense change in land use at Alta Floresta, which had no precedent during the Holocene history of the Amazon. High charcoal accumulation rates that were observed in the Carajás region during low lake level phases in the Amazon in the mid-Holocene were comparable to those at the onset of the human ... Mostrar Tudo |
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Thesagro: |
Carvão Vegetal. |
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Thesaurus Nal: |
Amazonia; Charcoal; Climate change. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/115554/1/cpamt-2014-rodrigues-palaeofires-amazon.pdf
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Marc: |
LEADER 03337naa a2200373 a 4500
001 2005589
005 2015-01-14
008 2014 bl uuuu u00u1 u #d
022 $a0031-0182
024 7 $ahttp://dx.doi.org.ez103.periodicos.capes.gov.br/10.1016/j.palaeo.2014.07.020$2DOI
100 1 $aCORDEIRO, R. C.
245 $aPalaeofires in Amazon$bInterplay between land use change and palaeoclimatic events$h[electronic resource]
260 $c2014
300 $a15
520 $aInterpreting the geological record of Amazon biomass combustion requires comparing charcoal accumulation rates in various biomes at different time scales. Charcoal accumulation rates, a proxy for palaeofire records, were obtained in sediment cores from Amazon lakes surrounded by several vegetation types and from a reservoirs in an intense land use change region. The records presented in this study were obtained in the following areas i) a reservoirs in Alta Floresta region (northern Mato Grosso State); ii) Lago do Saci (southern Pará State), a lake close to Alta Floresta and located at the southern border of Pará State; iii) a bog in an ecotone area in the Humaitá region (southern Amazonas State); iv) lakes in lateritic iron crust of the Carajás Hills (southeastern Pará State); v) Lago Comprido, a floodplain lake close to the Amazon River and surrounded by tropical rain forest (Monte Alegre, Pará State; vi) Lagoa da Pata in the Morro dos Seis Lagos alkaline complex (São Gabriel da Cachoeira, Amazonas State) and vii) Lago Caracaranã, a secluded lake in the northern Amazon cerrado (Roraima State). The highest charcoal accumulation rates were observed for modern records related to an intense change in land use at Alta Floresta, which had no precedent during the Holocene history of the Amazon. High charcoal accumulation rates that were observed in the Carajás region during low lake level phases in the Amazon in the mid-Holocene were comparable to those at the onset of the human settlement in Alta Floresta region. An increase in charcoal accumulation rate was observed in the late Holocene when the lake level was high, suggesting an interaction between climates and human presence. Low charcoal accumulation rates are typical of modern high rainfall environments, as observed in Lagoa da Pata where the environment is not susceptible to occurrences of wildfires even during relatively drier climatic phases. Low charcoal accumulation rates also exist in the relatively dry cerrado (savanna type) biome even during relatively dry phases in the Caracaranã region where the savanna-type vegetation biomass is lower and thus generates less charcoal particles than forest ecosystems.
650 $aAmazonia
650 $aCharcoal
650 $aClimate change
650 $aCarvão Vegetal
700 1 $aTURCQ, B.
700 1 $aMOREIRA, L. S.
700 1 $aRODRIGUES, R. de A. R.
700 1 $aSIMÕES FILHO, F. F. L.
700 1 $aMARTINS, G. S.
700 1 $aSANTOS, A. B.
700 1 $aBARBOSA, M.
700 1 $aCONCEIÇÃO, M. C. G. da
700 1 $aRODRIGUES, R. de C.
700 1 $aEVANGELISTA, H.
700 1 $aMOREIRA-TURCQ, P.
700 1 $aPENIDO, Y. P.
700 1 $aSIFEDDINE, A.
700 1 $aSEOANE, J. C. S.
773 $tPalaeogeography, Palaeoclimatology, Palaeoecology$gv. 415, p.137-151, dez. 2014
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Embrapa Agrossilvipastoril (CPAMT) |
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Registro Completo
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Biblioteca(s): |
Embrapa Caprinos e Ovinos. |
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Data corrente: |
28/04/2020 |
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Data da última atualização: |
10/08/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
PINTO, P. H. N.; BALARO, M. F. A.; SARAIVA, H. F. R. de A.; BRAIR, V. L.; ALFRADIQUE, V. A. P.; CÔRTESA, L. R.; COSENTINO, I. O.; SOUZA-FABJANA, J. M. G.; FONSECA, J. F. da; BRANDÃO, F. Z. |
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Afiliação: |
PEDRO HENRIQUE NICOLAU PINTO, Universidade Federal Fluminense; MARIO FELIPE ALVAREZ BALARO, Universidade Federal Fluminense; HELENA FABIANA REIS DE ALMEIDA SARAIVA, Universidade Federal Fluminense; VIVIANE LOPES BRAIR, Universidade Federal Fluminense; VIVIAN ANGÉLICO PEREIRA ALFRADIQUE, Universidade Federal Fluminense; LUANA RANGEL CÔRTESA, Universidade Federal Fluminense; ISABEL OLIVEIRA COSENTINO, Universidade Federal Fluminense; JOANNA MARIA GONCALVES SOUZA-FABJANA; JEFERSON FERREIRA DA FONSECA, CNPC; FELIPE ZANDONADI BRANDÃO, Universidade Federal Fluminense. |
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Título: |
Successive in vivo embryo production in Santa Inês sheep. |
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Ano de publicação: |
2020 |
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Fonte/Imprenta: |
Animal Production Science, v. 60, n. 4, p. 497-502, Dec. 2020. |
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DOI: |
https://doi.org/10.1071/AN18740 |
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Idioma: |
Inglês |
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Conteúdo: |
Abstract: Context. In vivoembryo production, also called multiple ovulation and embryo transfer, can accelerate genetic gain, andthus improve animal production. However, there are issues limiting a wider use of this biotechnology in sheep livestock.Aims.This study aimed to determine (1) whether a previous response to superovulation (SOV) can be used as a criterionto select ewes forin vivoembryo production, (2) whether the intensity of the SOV response (number of corpora lutea, CL)can affect the embryo recovery rate, and (3) whether the number of CL quantified by colour Doppler ultrasonography can beused to calculate the recovery rate.Methods.Twenty-five Santa Inês ewes underwent SOV three times (SOV1, SOV2 and SOV3), with 200 mg FSH andnatural mating. The number of CL after each SOV was determined by laparoscopy and by colour Doppler ultrasonography.Key results.The number of CL significantly decreased (P<0.05) after SOV1 (7.54.8) to 3.05.0 at SOV 2 and2.23.5 at SOV3. Strong correlations were observed between SOV2 and SOV3 in terms of numbers of CL (r= 0.86,r2= 0.74;P<0.0001) and viable embryos (r= 0.79,r2= 0.63;P<00001). However, no correlations were observed betweenSOV1 and SOV2 or between SOV1 and SOV3. Recovery rate did not differ with the intensity of the SOV response(6, 7?10,>10 CL) or between the methods used to quantify CL.Conclusions.Ewes did not show the same pattern of response when submitted to successive FSH-based SOV. Theintensity of the SOV response did not affect the recovery rate, and the number of CL estimated by colour Dopplerultrasonography can be used to calculate the recovery rate.Implications.Selecting sheep embryo donors by a previous SOV response is not always feasible. The recovery rate ishomogeneous and it is not affected by the intensity of the SOV response. A nonsurgical technique can be used to assess therecovery rate, improving animal welfare in MOET programs. MenosAbstract: Context. In vivoembryo production, also called multiple ovulation and embryo transfer, can accelerate genetic gain, andthus improve animal production. However, there are issues limiting a wider use of this biotechnology in sheep livestock.Aims.This study aimed to determine (1) whether a previous response to superovulation (SOV) can be used as a criterionto select ewes forin vivoembryo production, (2) whether the intensity of the SOV response (number of corpora lutea, CL)can affect the embryo recovery rate, and (3) whether the number of CL quantified by colour Doppler ultrasonography can beused to calculate the recovery rate.Methods.Twenty-five Santa Inês ewes underwent SOV three times (SOV1, SOV2 and SOV3), with 200 mg FSH andnatural mating. The number of CL after each SOV was determined by laparoscopy and by colour Doppler ultrasonography.Key results.The number of CL significantly decreased (P<0.05) after SOV1 (7.54.8) to 3.05.0 at SOV 2 and2.23.5 at SOV3. Strong correlations were observed between SOV2 and SOV3 in terms of numbers of CL (r= 0.86,r2= 0.74;P<0.0001) and viable embryos (r= 0.79,r2= 0.63;P<00001). However, no correlations were observed betweenSOV1 and SOV2 or between SOV1 and SOV3. Recovery rate did not differ with the intensity of the SOV response(6, 7?10,>10 CL) or between the methods used to quantify CL.Conclusions.Ewes did not show the same pattern of response when submitted to successive FSH-based SOV. Theintensity of the SOV response did not aff... Mostrar Tudo |
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Palavras-Chave: |
MOET; Ovarian superstimulation. |
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Thesagro: |
Corpo Lúteo; Melhoramento Genético Animal; Ovino; Reprodução Animal; Superovulação; Transferência de Embrião. |
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Thesaurus NAL: |
Animal reproduction; Breeding and Genetic Improvement; Corpus luteum; Embryo transfer; Ewes; Superovulation. |
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Categoria do assunto: |
G Melhoramento Genético |
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Marc: |
LEADER 03132naa a2200409 a 4500
001 2121864
005 2021-08-10
008 2020 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1071/AN18740$2DOI
100 1 $aPINTO, P. H. N.
245 $aSuccessive in vivo embryo production in Santa Inês sheep.$h[electronic resource]
260 $c2020
520 $aAbstract: Context. In vivoembryo production, also called multiple ovulation and embryo transfer, can accelerate genetic gain, andthus improve animal production. However, there are issues limiting a wider use of this biotechnology in sheep livestock.Aims.This study aimed to determine (1) whether a previous response to superovulation (SOV) can be used as a criterionto select ewes forin vivoembryo production, (2) whether the intensity of the SOV response (number of corpora lutea, CL)can affect the embryo recovery rate, and (3) whether the number of CL quantified by colour Doppler ultrasonography can beused to calculate the recovery rate.Methods.Twenty-five Santa Inês ewes underwent SOV three times (SOV1, SOV2 and SOV3), with 200 mg FSH andnatural mating. The number of CL after each SOV was determined by laparoscopy and by colour Doppler ultrasonography.Key results.The number of CL significantly decreased (P<0.05) after SOV1 (7.54.8) to 3.05.0 at SOV 2 and2.23.5 at SOV3. Strong correlations were observed between SOV2 and SOV3 in terms of numbers of CL (r= 0.86,r2= 0.74;P<0.0001) and viable embryos (r= 0.79,r2= 0.63;P<00001). However, no correlations were observed betweenSOV1 and SOV2 or between SOV1 and SOV3. Recovery rate did not differ with the intensity of the SOV response(6, 7?10,>10 CL) or between the methods used to quantify CL.Conclusions.Ewes did not show the same pattern of response when submitted to successive FSH-based SOV. Theintensity of the SOV response did not affect the recovery rate, and the number of CL estimated by colour Dopplerultrasonography can be used to calculate the recovery rate.Implications.Selecting sheep embryo donors by a previous SOV response is not always feasible. The recovery rate ishomogeneous and it is not affected by the intensity of the SOV response. A nonsurgical technique can be used to assess therecovery rate, improving animal welfare in MOET programs.
650 $aAnimal reproduction
650 $aBreeding and Genetic Improvement
650 $aCorpus luteum
650 $aEmbryo transfer
650 $aEwes
650 $aSuperovulation
650 $aCorpo Lúteo
650 $aMelhoramento Genético Animal
650 $aOvino
650 $aReprodução Animal
650 $aSuperovulação
650 $aTransferência de Embrião
653 $aMOET
653 $aOvarian superstimulation
700 1 $aBALARO, M. F. A.
700 1 $aSARAIVA, H. F. R. de A.
700 1 $aBRAIR, V. L.
700 1 $aALFRADIQUE, V. A. P.
700 1 $aCÔRTESA, L. R.
700 1 $aCOSENTINO, I. O.
700 1 $aSOUZA-FABJANA, J. M. G.
700 1 $aFONSECA, J. F. da
700 1 $aBRANDÃO, F. Z.
773 $tAnimal Production Science$gv. 60, n. 4, p. 497-502, Dec. 2020.
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