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How Many Seals Were There? The Global Shelf Loss during the Last Glacial Maximum and Its Effect on the Size and Distribution of Grey Seal Populations

机译:那里有多少封印?最后一次冰川最大时期的全球陆架损失及其对灰海豹种群数量和分布的影响

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摘要

Predicting how marine mammal populations respond to habitat changes will be essential for developing conservation management strategies in the 21st century. Responses to previous environmental change may be informative in the development of predictive models. Here we describe the likely effects of the last ice age on grey seal population size and distribution. We use satellite telemetry data to define grey seal foraging habitat in terms of the temperature and depth ranges exploited by the contemporary populations. We estimate the available extent of such habitat in the North Atlantic at present (between 1.42·106 km2 and 2.07·106 km2) and at the last glacial maximum (between 4.74·104 km2 and 2.11·105 km2); taking account of glacial and seasonal sea-ice coverage, estimated reductions of sea-level (123 m) and sea surface temperature hind-casts. Most of the extensive continental shelf waters (North Sea, Baltic Sea and Scotian Shelf), currently supporting >95% of grey seals, were unavailable during the last glacial maximum. A combination of lower sea-level and extensive ice-sheets, massively increased seasonal sea-ice coverage and southerly extent of cold water would have pushed grey seals into areas with no significant shelf waters. The habitat during the last glacial maximum might have been as small as 3% of today's extent and grey seal populations may have fallen to similarly low numbers. An alternative scenario involving a major change to a pelagic or bathy-pelagic foraging niche cannot be discounted. However, hooded seals currently dominate that niche and may have excluded grey seals from such habitat. If as seems likely, the grey seal population fell to very low levels it would have remained low for several thousand years before expanding into current habitats over the past 12,000 years or so.
机译:预测海洋哺乳动物种群对生境变化的反应对于21世纪制定保护管理策略至关重要。对先前环境变化的响应可能会在预测模型的开发中提供参考。在这里,我们描述了最后一次冰期对灰海豹种群数量和分布的可能影响。我们使用卫星遥测数据根据当代人口开发的温度和深度范围来定义灰海豹觅食栖息地。我们估计了目前北大西洋此类生境的可用范围(介于1.42·10 6 km 2 和2.07·10 6 km < sup> 2 )和最后一个冰期最大值(介于4.74·10 4 km 2 和2.11·10 5 km < sup> 2 );考虑到冰川和季节性海冰的覆盖范围,估计海平面(123 m)和海面温度下降的后兆减少。在上一次冰川最大时期,目前大部分支持> 95%灰海豹的大部分广泛的大陆架水域(北海,波罗的海和斯科蒂尔大陆架)都没有。较低的海平面和广泛的冰盖,季节性海冰覆盖面的大量增加以及南半球的冷水的结合,将使灰海豹进入没​​有大量积水的地区。上一次冰川最大期的栖息地可能只有今天的3%,灰海豹种群数量也可能下降到类似的低水平。涉及到上层或深水上层觅食生态位发生重大变化的替代方案是不能忽视的。但是,带帽海豹目前在该生态位中占主导地位,并且可能已将灰色海豹从此类栖息地中排除。如果看起来像这样,灰海豹种群下降到非常低的水平,那么在过去的12,000年左右的时间里,灰海豹种群在进入目前的栖息地之前将一直处于低水平。

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