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Plankton biomass and larval fish abundance prior to andduring the El Niño period of 1997–1998 along the central Pacific coast of México

机译:之前和之后浮游生物的生物量和幼体鱼的丰度在1997年至1998年的厄尔尼诺时期,沿墨西哥中部太平洋海岸

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摘要

The temporal and spatial distributions of zooplankton biomass and larval fish recorded during 27 months (December1995–December 1998) off the Pacific coast of central México are analyzed. A total of 316 samples were obtained by surface(from 40–68 to 0 m) oblique hauls at 12 sampling sites using a Bongo net. Two well-defined periods were observed: apre-ENSO period (December 1995–march 1997) and an ENSO event (July 1997–September 1998) characterized byimpoverishment of the pelagic habitat. The highest biomass concentrations occurred at coastal stations during thepre-ENSO period. During the El Nin˜o period no spatial patterns were found in coastal waters. The months with highestbiomass were those in which the lowest sea surface temperature (SST) occurred (January–May), and this pattern was alsoobserved during the ENSO period. A typical, although attenuated, seasonal environmental pattern with enhanced phytoplankton(diatoms and dinoflagellates) was prevalent during the El Nin˜o event in nearshore waters. During the El Niñoperiod the phytoplankton was mainly small diatoms (microphytoplankton), while dinoflagellates were practically absent.The most parsimonious generalized linear models explaining spatial and temporal distribution of larval fish speciesincluded the ENSO index (MEI), upwelling index (UI) and distance to the coast. The environmental variability definedon an interannual time-scale by the ENSO event and the seasonal hydroclimatic pattern defined by the UI (intra-annualscale)controlled the ecosystem productivity patterns. The small-scale distribution patterns (defined by a cross-shore gradient)of plankton were related to the hydroclimatic seasonality and modulated by interannual anomalies
机译:分析了墨西哥中部太平洋沿岸27个月(1995年12月至1998年12月)记录的浮游动物生物量和幼体鱼的时空分布。使用Bongo网在12个采样点通过斜向拖运(从40-68到0 m)获得了316个样本。观测到了两个明确的时期:ENSO前时期(1995年12月至1997年3月)和ENSO事件(1997年7月至1998年9月),其特征是中上层生境贫乏。在ENSO之前的时期内,沿海地区的生物量浓度最高。在厄尔尼诺现象期间,沿海水域未发现任何空间格局。生物量最高的月份是发生最低海面温度(SST)的月份(1月至5月),并且在ENSO期间也观察到了这种模式。在近海的厄尔尼诺事件期间,虽然浮游植物(硅藻和鞭毛藻)增强,但典型的季节性环境模式虽然减弱了,但仍很普遍。在厄尔尼诺期,浮游植物主要是小型硅藻(微浮游植物),而鞭毛藻几乎没有。最简约的广义线性模型解释了幼体鱼的时空分布,包括ENSO指数(MEI),向上上升指数(UI)和到鱼类的距离海岸。 ENSO事件在年际尺度上定义的环境变化和UI(年际尺度)上定义的季节性水气候模式控制了生态系统的生产力模式。浮游生物的小尺度分布模式(由跨岸梯度定义)与水文气候季节性有关,并受年际异常的影响

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