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Giant kelp (Macrocystis pyrifera) survival in deep water (25-40 m)during El Nino of 1997-1998 in Baja California, Mexico

机译:1997年至1998年在墨西哥下加利福尼亚州的厄尔尼诺现象期间,巨型海带(Macrocystis pyrifera)在深水(25-40 m)中的生存

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摘要

During the 1997-1998 El Nino, we examined seasonally a giant kelp population in deep water (25-40 m) off the coast of Northern Baja California. Though most populations in the region completely disappeared, large fertile adults survived the entire warming event at depth. At 25 m, there was no significant change in density or number of fronds per individual during the warming period from spring 1997 to spring 1998, though the surface canopy sloughed off (died) down to 15 m depth. By summer 1998, recruitment occurred at all depths at the site. Adult survival at depth was most likely important in post-disturbance recovery in surrounding populations by occupying substratum, providing vegetative growth, and producing spores. Survival in deep water during this extreme El Nino may have been due to local hydrography, such as internal waves bringing cool nitrate-rich water into the deeper regions of the shelf from below the thermocline, providing a refugium against the warm temperatures, low nutrients, and heavy wave action associated with warming events. Deep-water populations may regularly survive El Nino warming in this region due to internal wave activity, and go undetected due to the depth at which they occur and the sloughing of the shallow (15 m) biomass.
机译:在1997-1998年的厄尔尼诺现象期间,我们季节性研究了北下加利福尼亚州沿海深海(25-40 m)中的大量海带种群。尽管该地区的大多数人口完全消失了,但大量可育的成年人在整个变暖事件中都幸存下来。在1997年春季至1998年春季的升温期间,在25 m处,每个个体的密度或叶状体的数量没有显着变化,尽管表面冠层脱落(死亡)至15 m深度。到1998年夏季,该地点的所有深度都进行了招募。通过占领地下,提供营养生长并产生孢子,成年后深处的成年存活最有可能对周围人群进行干扰后恢复。在这种极端的厄尔尼诺现象期间,深水中的生存可能是由于局部水文学造成的,例如内部波将冷的富含硝酸盐的水从温水线下方带入架子的较深区域,从而为温暖的温度,低养分提供了避难所,以及与变暖事件相关的强波浪作用。由于内部波浪活动,深水种群可能定期在该地区的厄尔尼诺变暖中幸存下来,而由于它们发生的深度和浅(<15 m)生物质的塌陷而未被发现。

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