Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, Athens, Ohio, United States of America.
PLoS One. 2010 Dec 29;5(12):e15584. doi: 10.1371/journal.pone.0015584.
During the Late Devonian Biodiversity Crisis, the primary driver of biodiversity decline was the dramatic reduction in speciation rates, not elevated extinction rates; however, the causes of speciation decline have been previously unstudied. Speciation, the formation of new species from ancestral populations, occurs by two primary allopatric mechanisms: vicariance, where the ancestral population is passively divided into two large subpopulations that later diverge and form two daughter species, and dispersal, in which a small subset of the ancestral population actively migrates then diverges to form a new species. Studies of modern and fossil clades typically document speciation by vicariance in much higher frequencies than speciation by dispersal. To assess the mechanism behind Late Devonian speciation reduction, speciation rates were calculated within stratigraphically constrained species-level phylogenetic hypotheses for three representative clades and mode of speciation at cladogenetic events was assessed across four clades in three phyla: Arthropoda, Brachiopoda, and Mollusca. In all cases, Devonian taxa exhibited a congruent reduction in speciation rate between the Middle Devonian pre-crisis interval and the Late Devonian crisis interval. Furthermore, speciation via vicariance is almost entirely absent during the crisis interval; most episodes of speciation during this time were due to dispersal. The shutdown of speciation by vicariance during this interval was related to widespread interbasinal species invasions. The lack of Late Devonian vicariance is diametrically opposed to the pattern observed in other geologic intervals, which suggests the loss of vicariant speciation attributable to species invasions during the Late Devonian was a causal factor in the biodiversity crisis. Similarly, modern ecosystems, in which invasive species are rampant, may be expected to exhibit similar shutdown of speciation by vicariance as an outcome of the modern biodiversity crisis.
在晚泥盆世生物多样性危机期间,生物多样性下降的主要驱动因素是物种形成率的急剧下降,而不是灭绝率的升高;然而,物种形成率下降的原因以前尚未研究过。物种形成是指从祖先种群中形成新物种的过程,主要通过两种异域机制发生:隔离,即祖先种群被动地分裂成两个大的亚种群,然后它们分化形成两个后代物种;以及扩散,其中一小部分祖先种群主动迁移,然后分化形成一个新物种。对现代和化石进化枝的研究通常记录到,通过隔离发生的物种形成比通过扩散发生的物种形成频率更高。为了评估晚泥盆世物种形成减少的机制,在三个代表进化枝的地层约束物种水平系统发育假设内计算了物种形成率,并在三个门的四个进化枝中评估了谱系分化事件的物种形成模式:节肢动物、腕足动物和软体动物。在所有情况下,泥盆纪类群在中泥盆世危机前间隔和晚泥盆世危机间隔之间表现出一致的物种形成率降低。此外,在危机间隔期间,通过隔离发生的物种形成几乎完全不存在;在此期间大多数物种形成事件归因于扩散。在此期间隔离物种形成的关闭与广泛的盆地间物种入侵有关。在这个间隔期间缺乏晚泥盆世的隔离与在其他地质间隔期间观察到的模式截然相反,这表明归因于晚泥盆世物种入侵的隔离物种形成的丧失是生物多样性危机的一个因果因素。同样,在现代生态系统中,入侵物种猖獗,可能会预期由于现代生物多样性危机而出现类似的隔离物种形成关闭。