全球生物多样性的观测模式

B. Worm, D. Tittensor
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引用次数: 0

摘要

本章总结和综合了已知的生物多样性模式,并分析了它们在空间和时间上的一致性。讨论仅限于大陆到全球尺度(数千公里)的宏观生态模式。本章还着重于生物多样性最简单的衡量标准——即物种丰富度。讨论内容包括海洋沿海生物多样性、海洋中上层生物多样性、深海生物多样性、陆地生物多样性、生物多样性模式的时空变化以及文献记载的生物多样性模式的稳健性。研究发现,在陆地和海洋上所有已知的物种群中,热带物种丰富度的峰值与亚热带物种丰富度的峰值一样常见,而温带或极地纬度的物种群则更为罕见。因此,经常被引用的生物多样性单峰模式经常出现,特别是在陆地上,但也有证据支持一种新出现的不对称单峰或双峰模式,这种模式经常出现在亚热带地区,特别是在海洋领域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observed Patterns of Global Biodiversity
This chapter summarizes and synthesizes known biodiversity patterns, and analyzes them for congruency over space and time. The discussion is limited to macroecological patterns at continental to global scales (thousands of km). The chapter also focuses on the simplest measure of biodiversity—namely, species richness. The discussions cover marine coastal biodiversity, marine pelagic biodiversity, deep-sea biodiversity, terrestrial biodiversity, changes in biodiversity patterns through time, and robustness of documented biodiversity patterns. Among the findings is that averaging across all known species groups on land and in the sea, tropical peaks in species richness were as common as subtropical peaks, whereas species groups cresting in temperate or polar latitudes were more exceptional. Thus, the oft-cited unimodal pattern of biodiversity appears frequently, particularly on land, but there is also evidence that supports a newly emerging paradigm of asymmetric unimodal or bimodal peaks often in the subtropics, and particularly in the marine realm.
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