The impact of climate on biodiversity is indisputable. Climate changes over geological time must have significantly influenced the evolution of biodiversity, ultimately leading to its present pattern. Here we consider the paleoclimate data record, inferring that present-day hot and cold environments should contain, respectively, the largest and the smallest diversity of ancestral lineages of microbial eukaryotes.
We investigate this hypothesis by analyzing an original dataset of 18S rRNA gene sequences from Western Greenland in the Arctic, and data from the existing literature on 18S rRNA gene diversity in hydrothermal vent, temperate sediments, and anoxic water column communities. Unexpectedly, the community from the cold environment emerged as one of the richest observed to date in protistan species, and most diverse in ancestral lineages.
This pattern is consistent with natural selection sweeps on aerobic non-psychrophilic microbial eukaryotes repeatedly caused by low temperatures and global anoxia of snowball Earth conditions. It implies that cold refuges persisted through the periods of greenhouse conditions, which agrees with some, although not all, current views on the extent of the past global cooling and warming events. We therefore identify cold environments as promising targets for microbial discovery.
climate, biodiversity, Arctic, rRNA, paleoclimate, microbial eukaryotes
Biodiversity - Climatic factors, Protista - Arctic Ocean
Biodiversity | Microbiology
Public Library of Science
This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Thorsten Stoeck, et al.
Stoeck, Thorsten; Kasper, Jennifer; Bunge, John; Leslin, Chesley; Ilyin, Valya; and Epstein, Slava S., "Protistan diversity in the arctic: a case of paleoclimate shaping modern biodiversity?" (2007). Biology Faculty Publications. Paper 21. http://hdl.handle.net/2047/d20002448
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