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年龄和面积预测了浮石筏中物种丰富度的模式,这取决于所遇到的海洋气候带。

Age and area predict patterns of species richness in pumice rafts contingent on oceanic climatic zone encountered.

作者信息

Velasquez Eleanor, Bryan Scott E, Ekins Merrick, Cook Alex G, Hurrey Lucy, Firn Jennifer

机构信息

School of Earth Environmental and Biological Sciences Faculty of Science and Engineering Queensland University of Technology Brisbane Qld Australia.

Queensland Museum Brisbane Qld Australia.

出版信息

Ecol Evol. 2018 Apr 24;8(10):5034-5046. doi: 10.1002/ece3.3980. eCollection 2018 May.

Abstract

The theory of island biogeography predicts that area and age explain species richness patterns (or alpha diversity) in insular habitats. Using a unique natural phenomenon, pumice rafting, we measured the influence of area, age, and oceanic climate on patterns of species richness. Pumice rafts are formed simultaneously when submarine volcanoes erupt, the pumice clasts breakup irregularly, forming irregularly shaped pumice stones which while floating through the ocean are colonized by marine biota. We analyze two eruption events and more than 5,000 pumice clasts collected from 29 sites and three climatic zones. Overall, the older and larger pumice clasts held more species. Pumice clasts arriving in tropical and subtropical climates showed this same trend, where in temperate locations species richness (alpha diversity) increased with area but decreased with age. Beta diversity analysis of the communities forming on pumice clasts that arrived in different climatic zones showed that tropical and subtropical clasts transported similar communities, while species composition on temperate clasts differed significantly from both tropical and subtropical arrivals. Using these thousands of insular habitats, we find strong evidence that area and age but also climatic conditions predict the fundamental dynamics of species richness colonizing pumice clasts.

摘要

岛屿生物地理学理论预测,面积和年代可以解释岛屿栖息地的物种丰富度模式(即α多样性)。我们利用浮石漂流这一独特的自然现象,测量了面积、年代和海洋气候对物种丰富度模式的影响。浮石筏在海底火山爆发时同时形成,浮石碎屑不规则破碎,形成形状不规则的浮石,这些浮石在海洋中漂浮时会被海洋生物群落定殖。我们分析了两次火山喷发事件以及从29个地点和三个气候带收集的5000多个浮石碎屑。总体而言,年代越久、体积越大的浮石碎屑拥有的物种越多。抵达热带和亚热带气候区的浮石碎屑也呈现出相同趋势,而在温带地区,物种丰富度(α多样性)随面积增加而增加,但随年代增长而降低。对在不同气候带抵达的浮石碎屑上形成的群落进行的β多样性分析表明,热带和亚热带的浮石碎屑携带的群落相似,而温带浮石碎屑上的物种组成与热带和亚热带抵达的浮石碎屑有显著差异。利用这数千个岛屿栖息地,我们发现有力证据表明,面积、年代以及气候条件都能预测定殖在浮石碎屑上的物种丰富度的基本动态。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0aa7/5980578/c6810ffdf09e/ECE3-8-5034-g001.jpg

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