Anthony Colin J, Bentlage Bastian, Helm Rebecca R
Marine Laboratory, University of Guam, Mangilao, Guam 96913, USA.
Earth Commons Institute, Georgetown University, Washington, DC 20057, USA.
Curr Biol. 2024 Jan 8;34(1):196-203.e2. doi: 10.1016/j.cub.2023.11.013.
Innovation is a key to evolutionary success and entrance into novel ecosystems. Species that float freely at the ocean's surface, termed obligate neuston (also called pleuston, here referred to simply as neuston), include highly specialized taxa from distinct evolutionary lineages that evolved floating morphologies. In 1958, Soviet scientist, A.I. Savilov, stated that floating animal species are derived from benthic ancestors, rather than species from the adjacent pelagic zone, and that floating morphologies are homologous to benthic attachment structures. To test Savilov's hypothesis, we constructed molecular phylogenies and ancestral states for all major floating groups for which molecular data were available. Our results reveal that four of the five clades examined arose directly from a substrate-attached ancestor, although that substrate was not necessarily the benthos, as Savilov stated, and instead included epibiotic and rafting ancestors. Despite their diverse evolutionary origins, floating animals use gas-trapping mechanisms to remain at the surface, and many of these gas-trapping structures appear to be homologous to substrate attachment structures. We also reconstruct the trophic habits of floating mollusks and their sister species, revealing that prey preference remains conserved upon entering the ocean's surface ecosystem. Colonization of the ocean's surface seems to have occurred through successive evolutionary steps from the seafloor. Our results suggest that these steps often included transitions through epibiotic (where species attach to other living organisms) or rafting (where species attach to floating debris) habits. The water-air interface, despite its unique properties, may, in some ways, be just another substrate.
创新是进化成功和进入新生态系统的关键。自由漂浮在海洋表面的物种,被称为专性漂浮生物(也称为漂浮生物,这里简称为漂浮生物),包括来自不同进化谱系的高度特化分类群,它们进化出了漂浮形态。1958年,苏联科学家A.I.萨维洛夫指出,漂浮动物物种起源于底栖动物祖先,而非相邻的远洋区物种,并且漂浮形态与底栖附着结构同源。为了验证萨维洛夫的假设,我们构建了所有有分子数据可用的主要漂浮类群的分子系统发育树和祖先状态。我们的结果表明,所研究的五个进化枝中有四个直接起源于附着在基质上的祖先,尽管该基质不一定如萨维洛夫所说的是底栖生物,而是包括体表共生和漂流祖先。尽管它们有着不同的进化起源,但漂浮动物利用气体捕获机制停留在水面,而且许多这些气体捕获结构似乎与基质附着结构同源。我们还重建了漂浮软体动物及其姊妹物种的营养习性,揭示了进入海洋表面生态系统后猎物偏好仍然保持不变。海洋表面的定殖似乎是通过从海底连续的进化步骤发生的。我们的结果表明,这些步骤通常包括通过体表共生(物种附着在其他生物体上)或漂流(物种附着在漂浮碎片上)习性的转变。水 - 气界面尽管具有独特性质,但在某些方面可能只是另一种基质。