加勒比海沿岸生态系统的演变和环境
Jeremy B C Jackson1,2, Aaron O'Dea2,3
1Division of Paleontology, American Museum of Natural History, New York, NY 10024-5192.
概括
巴拿马的地峡巴拿马的地峡
科学领域:
- 海洋生物学 海洋生物学
- 古海洋学是古海洋学.
- 进化生态学的进化生态学
背景情况:
- 在普略纪晚期巴拿马半岛的关闭使加勒比海与东太平洋隔绝.
- 这一地质事件导致了加勒比地区的重大生物转移和灭绝,但驱动因素仍然不清楚.
研究的目的:
- 为了调查历史海洋学变化对加勒比海生物群的影响,巴拿马峡的关闭后.
- 测试将环境变化,特别是减少的上游,与海洋社区的生物反应联系在一起的假设.
主要方法:
- 分析历史海洋学数据,包括温度波动,以推断上升强度的变化.
- 将环境变化与海洋物种养生态,生命历史和息地的记录变化相关联.
- 检查生物变化的空间模式,并应用元人口理论来理解灭绝动态.
主要成果:
- 海洋上游强度的急剧下降被确定为一个关键的环境变化.
- 减少上游导致悬浮食者和捕食者的数量减少.
- 海草和珊瑚礁息地的扩散,以及无脊椎动物的繁殖策略的转变,发生在超过100万年的时间滞后后.
结论:
- 由于巴拿马半岛关闭,上游的减少大大重组了加勒比海的海洋生态系统.
- 生物反应,包括息地变化和生命历史转移,表现出相当大的时间滞后,受灭绝债务等因素的影响.
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