Influence of hydrological changes on the composition of phytoplankton and sediment diatoms in the Rio de la Plata estuary

被引:0
|
作者
Martinez Goicoechea, Ana [1 ]
Perez, Laura [2 ]
Garcia-Rodriguez, Felipe [2 ,3 ]
机构
[1] Direcc Nacl Recursos Acuat MGAP DINARA, La Paloma, Uruguay
[2] Ctr Univ Reg Este UDELAR CURE, Rocha, Uruguay
[3] Univ Fed Rio Grande FURG, Inst Oceanog, Rio Grande, Brazil
关键词
Estuary; climate variability; ENSO; benthic-pelagic domains; microalgae; dinoflagellates; SOUTH-AMERICA; SOUTHWESTERN ATLANTIC; RIVER DISCHARGE; SPRING PHYTOPLANKTON; CONTINENTAL SHELVES; ORGANIC-MATTER; MARINE DIATOMS; WATER MASSES; VARIABILITY; COASTAL;
D O I
10.1080/00288330.2024.2307939
中图分类号
S9 [水产、渔业];
学科分类号
0908 ;
摘要
ENSO phases produce changes in precipitation and river flow in Eastern South America. We aimed to evaluate phytoplankton and surface sediment diatoms' response to ENSO within the Rio de la Plata estuary. A 180-km-long transect off the Uruguayan coast was undertaken in May 2009 (La Nina) and May 2010 (El Nino), where physical, chemical and biological variables were measured. During El Nino we registered lower temperatures/salinities throughout the transect, and the riverine zone was specifically more homogeneous in terms of temperature, salinity, turbidity and chlorophyll-a than during La Nina. We observed changes in the species composition of both planktonic and sediment diatoms. Concomitantly, a significant depletion in planktonic diatom abundance and richness in both planktonic and benthic domain during El Nino was observed. In addition, there was a higher proportion of dinoflagellates than during La Nina, which was explained by a higher water column stability. The dominance of the chain-forming and meso-eutrophic diatom Aulacoseira was registered during El Nino in both domains, mainly in the fluvial zone, related to a high river discharge. Our findings are important to anticipate changes in microalgae composition related to oceanographic variability during potential ENSO events.
引用
收藏
页码:678 / 700
页数:23
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