自2015年以来,在萨尔加索海北部的萨尔加索鱼种群急剧减少
Yingjun Zhang1, Brian B Barnes1, Deborah S Goodwin2
1College of Marine Science, University of South Florida, St. Petersburg, FL USA.
概括
自2015年以来,萨尔加索海的气量已经下降,生物质峰值因大大西洋气带的转移而发生变化. 这可能意味着萨尔加索分布的体制发生了变化.
科学领域:
- 海洋生物学 海洋生物学
- 海洋学 海洋学 海洋学
- 遥感是一种远程传感.
背景情况:
- 萨尔加索海是一个独特的海上生态系统,由漂浮的藻Sargassum定义.
- 大大西洋石灰带于2011年出现,扩大了石灰在热带大西洋的存在.
研究的目的:
- 调查2011年以后在萨尔加索海北部的萨尔加索海丰度和分布的变化.
- 了解萨尔加索姆季节性生长周期观察到的变化背后的驱动因素.
主要方法:
- 对卫星图像进行分析,以追踪石分布.
- 利用现场数据来评估石生物质和季节性循环.
- 石灰岩变化的相关性与海洋学因素,如海面温度.
主要成果:
- 自2015年以来,北萨尔加索海萨尔加索海的数量急剧减少.
- 破坏了Sargassum历史季节性生长周期,峰值从秋冬转移到春夏.
- 证据表明,沙加索从大西洋沙加索带向北沙加索海的 Sargassum 转移.
结论:
- 墨西哥湾Sargassum供应减少,可能与海面温度上升和海洋热浪有关,这可能是北萨尔加索海减少的原因.
- 大西洋大石带的石扩散和北沙加索海的下降的对比趋势表明石分布模式的潜在政权转变.
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