ABSTRACT
The forest dynamics in the Amazonian floodplains is strongly triggered by the flood pulse. Trees respond to unfavorable growth conditions during the flood period by cambial dormancy, which results in the formation of annual growth rings. We determined tree age and compared the mean annual rates of increase in the diameter of Macrolobium acaciifolium with hydrological and climatic factors in three regions of central Amazonian floodplain forest. A wood sample was obtained from each tree using an increment borer. Ring growth was assessed by marginal parenchyma bands to determine tree age and the mean diameter increment. Ring widths were indexed to construct cross-dating chronologies and correlated with climatic and hydrological variables. The analyses demonstrate that the mean annual diameter increment did not differ between the three study sites. The chronologies correlated significantly with the terrestrial phase. There was no significant difference in the ring-width index between El Niño years and other years, and between La Niña and other years. These results show that the hydrological variables can be considered crucial to the rates of tree growth and diameter increment in floodplains, and El Niño signals were not detected in the tree-ring chronologies.
A dinâmica das florestas alagáveis da Amazônia é fortemente influenciada pelo pulso anual de inundação. As árvores respondem às condições de crescimento desfavoráveis durante o período de inundação através da dormência cambial, resultando na formação de anéis de crescimento anuais. Neste estudo, determinamos a idade das árvores e comparamos as taxas anuais médias de incremento em diâmetro de Macrolobium acaciifolium com fatores hidrológicos e climáticos em três regiões de florestas alagáveis na Amazônia central. Para cada árvore, uma amostra de madeira foi obtida usando uma broca dendrocronológica. O crescimento do anel foi avaliado por bandas de parênquima marginal, para determinar a idade da árvore e o incremento médio em diâmetro. As séries de anéis foram indexadas, para construir cronologias, e correlacionadas com variáveis climáticas e hidrológicas. Nossas análises demonstraram que o incremento anual médio em diâmetro não diferiu entre os três locais de estudo. As cronologias correlacionaram-se significativamente com a fase terrestre. Não houve diferença significativa no índice de largura dos anéis entre os anos de El Niño e outros anos, e entre os anos de La Niña e outros anos. Estes resultados mostraram que as variáveis hidrológicas podem ser consideradas cruciais para as taxas de crescimento e de incremento em diâmetro das árvores em florestas alagáveis, e que não foram detectados sinais de El Niño nas cronologias das árvores analisadas.
Subject(s)
Water Cycle , Climate Effects/analysis , Life Cycle Stages , Fabaceae/growth & development , Abiotic Factors/analysis , Brazil , Amazonian EcosystemABSTRACT
The impacts of anomalous events in the Pacific Ocean associated with the El Niño - Southern Oscillation (ENSO) on rainfall over northern and northeastern regions of South America were evaluated for the period from 1900 to 2007 using composite analyses. The El Niño (La Niña) events in the Pacific, that together with a cold (warm) Atlantic Equatorial Mode (AEM) form an interbasin gradient between the Pacific and Atlantic were analyzed considering separately those for which the gradient forms during the ENSO onset phase from those for which the gradient forms during the ENSO demise phase. The results show that the rainfall pattern over the northern and northeastern region of South America is reinforced under an interbasin gradient during the initial phase of the ENSO event. In this case, a possible explanation is that the AEM with opposite sign of the ENSO event in its onset stage creates favorable conditions for the development of an interhemispheric gradient in the Tropical Atlantic acting in the same direction of the interbasin gradient, and collaborating to reinforce the El Niño (La Niña) effect on the precipitation. On the other hand, for ENSO events for which the interbasin gradient forms in the demise stage, the impact on the precipitation is more significative in the northern and central-western regions of the basin. A possible explanation for these differences is linked to the alterations in the east-west atmospheric circulation associated with the east-west gradient of the SST anomalies. The result of this study might be useful mainly for climate monitoring purposes.
Os impactos de eventos anômalos no oceano Pacífico associados ao El Niño-Oscilação Sul (ENOS) na precipitação da região norte e nordeste da América do Sul foram avaliados para o período de 1900 a 2007, fazendo-se uso de análise de composições. Os eventos El Niño (La Niña) no Pacífico que juntamente com um Modo Equatorial no Atlântico (MEA) frio (quente) formam um gradiente interbacias entre o Pacífico e Atlântico foram analisados considerando, separadamente, aqueles para os quais o gradiente se forma na fase inicial do ENOS daqueles em que o gradiente se forma na fase de decaimento do ENOS. Os resultados mostram que o padrão de precipitação na região norte e nordeste da América do Sul é reforçado mediante a configuração do gradiente interbacias durante a fase inicial do ENOS. Nesse caso, uma possível explicação é que o MEA de sinal contrário ao ENOS durante sua fase inicial cria condições favoráveis para o desenvolvimento de um gradiente inter-hemisférico no Atlântico Tropical atuando no mesmo sentido do gradiente interbacias, e colaborando para fortalecer o efeito do El Niño (La Niña) na precipitação. Por outro lado, para os eventos ENOS em que o gradiente se forma em sua fase de decaimento, o impacto na precipitação é mais significativo na região norte e centro-oeste da bacia. Uma possível explicação para essas diferenças está associada às mudanças que ocorrem na circulação atmosférica leste-oeste associada ao gradiente leste-oeste de anomalias da TSM. Os resultados deste estudo podem ser úteis, principalmente, para fins de monitoramento climático.
ABSTRACT
Present work investigated the relationship between Chlorophyll (Chl), of phytoplankton biomass, and sea surface temperature (SST) of the Black Sea, using Sea-viewing Wide Field-of-view Sensor (SeaWiFS) and Advanced Very High Resolution Radiometer (AVHRR) satellite imagery. Satellite derived data could provide information on the amount of sea life present (Brown algae, called kelp, proliferate, supporting new species of sea life, including otters, fish, and various invertebrates) in a given area throughout the world. SST from AVHRR from 1993 to 2008 showed seasonal, annual and interannual variability of temperature, monthly variability Chl from SeaWiFS from 1997 to 2009 has also been investigated. Chl showed two high peaks for the year 1999 and 2008. The correlation between SST and Chl for the same time has been found to be 60%. Correlation was significant at p<0.05. The information could also be useful in connection with studies of global changes in temperature and what effect they could have on the total abundance of marine life.
ABSTRACT
Megapitaria squalida (Bivalvia: Veneridae) fishery landings and temperature relationship in Bahía de la Paz, México. The clam Megapitaria squalida is a fishing resource with increasing importance in Northwestern Mexico. Nevertheless, this fishery has shown important variations that could be related to environmental factors. To assess this, monthly landings of M. squalida were analyzed during 2002-2005 for Bahía de La Paz, B.C.S., and were related with monthly time series of sea surface temperature, derived from MODIS-Aqua Sensor. The results showed a positive and significant relationship between sea surface temperature and clam landings. The likely impact of anomalous conditions of sea temperature on this resource is discussed. Rev. Biol. Trop. 59 (1): 151-157. Epub 2011 March 01.
La almeja chocolate Megapitaria squalida es un recurso pesquero con creciente importancia en el noroeste de México al registrarse un incremento en los volúmenes de captura. Sin embargo, esta pesquería ha observado variaciones importantes en las capturas que podrían estar relacionadas con factores ambientales. Se obtuvieron datos mensuales de producción de M. squalida durante 2002- 2005 y se estimaron series de tiempo de temperatura superficial del mar en la Bahía de La Paz B.C.S. a partir de imágenes mensuales derivadas del sensor MODIS-Aqua. Los resultados indican una relación positiva significativa entre la temperatura superficial del mar y los volúmenes de captura, razón por la cual nuestro trabajo tiene como objetivo estudiar las relaciones entre capturas de Megapitaria squalida (Bivalvia: Veneridae) y la temperatura superficial del mar en La Bahía de la Paz, Baja California Sur, México.
Subject(s)
Animals , Bivalvia/classification , Fisheries , Temperature , Mexico , Oceans and Seas , Population Density , Population Dynamics , SeasonsABSTRACT
Reproduction, diet and fishery of Octopus (Octopus) hubbsorum (Mollusca: Cephalopoda) in the coast of Oaxaca, Mexico. The octopus Octopus hubbsorum (Berry 1953) ranges widely and is important for the artisanal fishery in Puerto Angel, Oaxaca, Mexico. Samples were taken approximately at every two weeks from January 2002 to November 2003. All organisms were measured for dorsal mantle length (DLM) and total weight; sex and maturity gonadic stage were registered. For the stomach content analysis, frequency of occurrence and emptying indexes were used. The 352 organisms caught ranged from 4 to 18 cm in DLM; the sex ratio was different from 1 (X² = 24.2, p<0.05) throughout the year. The maximum values of the GSI appeared in May (4.1917 for females; 1.2675 in males). LDM for first sexual maturity (LDM50%) was 16 cm (females) and 14 cm (males). Octopus hubbsorum moves from deep waters to the coast, probably in search of better conditions, and lays masses of eggs on rocky substrata. They are fished from March to October, with higher intensity in April and May. Fishing effort was related to the oceanographic characteristics and the atmospheric conditions of the area. From April to September the CPUE monthly mean was 20-10 kg/divers/day. Using the CPUE and environmental condition relationship, the estimated adequate superficial temperature for fishing is 29.5 °C. Rev. Biol. Trop. 57 (1-2): 63-78. Epub 2009 June 30.
Se analizan algunos aspectos de la biología y pesquería de Octopus hubbsorum capturado por pesca artesanal en Puerto Ángel, Oaxaca, México. Las muestras se obtuvieron de enero 2002 a noviembre 2003 con una periodicidad quincenal. A cada uno de los organismos se les registró la longitud dorsal del manto (LDM), peso total, sexo y estado de madurez gonádica. Asímismo se obtuvo el Índice Gonadosomático (IGS). Para el análisis del contenido estomacal se utilizaron los índices de frecuencia de presencia y vaciado. Se analizaron 352 organismos, con un intervalo de tallas de 4 a 19 cm LDM; la proporción de sexos fue diferente de 1 (.2= 24.2, p<0.05) todo el año. Los valores máximos del IGS se presentaron en mayo (4.1917 hembras; 1.2675 machos). La LDM de primera madurez sexual para las hembras es de 16 cm (machos 14 cm). Octopus hubbsorum viaja a la costa con el fin de colocar las masas de huevos sobre sustratos rocosos y probablemente en busca de condiciones más adecuadas que a mayores profundidades. La pesca se realiza todo el año con un incremento en las capturas de marzo a octubre, con mayor intensidad en abril y mayo. El esfuerzo de pesca se encuentra relacionado con las características oceanográficas y las condiciones atmosféricas de la zona. De abril a septiembre la captura por unidad de esfuerzo (CPUE) promedio mensual varió entre 10 y 20 kg/buzo/día. A partir de la relación entre la CPUE y las variables ambientales, se estimó una temperatura superficial del mar (TSM) óptima, la cual es de 29.5 °C para la captura de esta especie.