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Seasonal sea ice cover as principal driver of spatial and temporal variation in depth extension and annual production of kelp in Greenland

机译:季节性海冰覆盖是格陵兰海带深度扩展和海藻年产量的时空变化的主要驱动力

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摘要

We studied the depth distribution and production of kelp along the Greenland coast spanning Arctic to sub-Arctic conditions from 78 oN to 64 oN. This covers a wide range of sea ice conditions and water temperatures, with those presently realized in the south likely to move northwards in a warmer future. Kelp forests occurred along the entire latitudinal range, and their depth extension and production increased southwards presumably in response to longer annual ice-free periods and higher water temperature. The depth limit of 10% kelp cover was 9-14 m at the northernmost sites (77-78 oN) with only 94-133 ice-free days per year, but extended to depths of 21-33 m further south (73 oN-64 oN) where >160 days per year were ice-free, and annual production of Saccharina longicruris and S. latissima, measured as the size of the annual blade, ranged up to sevenfold among sites. The duration of the open-water period, which integrates light and temperature conditions on an annual basis, was the best predictor (relative to summer water temperature) of kelp production along the latitude gradient, explaining up to 92% of the variation in depth extension and 80% of the variation in kelp production. In a decadal time series from a high Arctic site (74 oN), inter-annual variation in sea ice cover also explained a major part (up to 47%) of the variation in kelp production. Both spatial and temporal data sets thereby support the prediction that northern kelps will play a larger role in the coastal marine ecosystem in a warmer future as the length of the open-water period increases. As kelps increase carbon-flow and habitat diversity, an expansion of kelp forests may exert cascading effects on the coastal Arctic ecosystem. © 2012 Blackwell Publishing Ltd.
机译:我们研究了格陵兰岛沿海域从78 oN到64 oN的海带的深度分布和产量。这涵盖了广泛的海冰条件和水温,目前在南部实现的条件可能会在更温暖的未来向北移动。海带森林遍及整个纬度范围,其深度扩展和产量向南增加,可能是由于更长的年度无冰期和更高的水温所致。最北端的海带覆盖深度限制为9-14 m(77-78 oN),每年只有94-133天无冰天,但向南扩展至21-33 m(73 oN- 64 oN),其中每年> 160天无冰,而按年叶片大小衡量的Saccharina longicruris和S. latissima的年产量在不同地点之间的变化高达七倍。开放水域的持续时间是每年对光照和温度条件进行整合的时间,是沿纬度梯度海带生产的最佳预测指标(相对于夏季水温),可解释多达92%的深度扩展变化海带产量变化的80%。在北极高地(74 oN)的十年时间序列中,海冰覆盖的年际变化也解释了海带产量变化的主要部分(最高47%)。空间和时间数据集都支持这样的预测:随着开放水域时间的延长,北部海带在更温暖的未来将在沿海海洋生态系统中发挥更大的作用。随着海带增加碳流量和生境多样性,海带森林的扩张可能对沿海北极生态系统产生连锁效应。 ©2012布莱克威尔出版有限公司。

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