Byrne H M, Green J A M, Balbus S A, Ahlberg P E
School of Ocean Sciences, Bangor University, Menai Bridge, UK.
Department of Organismal Biology, Uppsala University, Uppsala, Sweden.
Proc Math Phys Eng Sci. 2020 Oct;476(2242):20200355. doi: 10.1098/rspa.2020.0355. Epub 2020 Oct 21.
Tides are a major component of the interaction between the marine and terrestrial environments, and thus play an important part in shaping the environmental context for the evolution of shallow marine and coastal organisms. Here, we use a dedicated tidal model and palaeogeographic reconstructions from the Late Silurian to early Late Devonian (420 Ma, 400 Ma and 380 Ma, Ma = millions of years ago) to explore the potential significance of tides for the evolution of osteichthyans (bony fish) and tetrapods (land vertebrates). The earliest members of the osteichthyan crown-group date to the Late Silurian, approximately 425 Ma, while the earliest evidence for tetrapods is provided by trackways from the Middle Devonian, dated to approximately 393 Ma, and the oldest tetrapod body fossils are Late Devonian, approximately 373 Ma. Large tidal ranges could have fostered both the evolution of air-breathing organs in osteichthyans to facilitate breathing in oxygen-depleted tidal pools, and the development of weight-bearing tetrapod limbs to aid navigation within the intertidal zones. We find that tidal ranges over 4 m were present around areas of evolutionary significance for the origin of osteichthyans and the fish-tetrapod transition, highlighting the possible importance of tidal dynamics as a driver for these evolutionary processes.
潮汐是海洋与陆地环境相互作用的一个主要组成部分,因此在塑造浅海和沿海生物进化的环境背景方面发挥着重要作用。在此,我们使用一个专门的潮汐模型以及从晚志留世到泥盆纪晚期早期(4.2亿年前、4.0亿年前和3.8亿年前,Ma = 百万年前)的古地理重建,来探究潮汐对硬骨鱼类(硬骨鱼)和四足动物(陆地脊椎动物)进化的潜在意义。硬骨鱼冠群的最早成员可追溯到晚志留世,约4.25亿年前,而四足动物的最早证据是来自泥盆纪中期的足迹化石,可追溯到约3.93亿年前,最古老的四足动物实体化石是泥盆纪晚期的,约3.73亿年前。大潮差可能既促进了硬骨鱼呼吸空气器官的进化,以便在缺氧的潮汐池中呼吸,也促进了四足动物承重肢体的发育,以帮助在潮间带内活动。我们发现,在硬骨鱼起源和鱼类 - 四足动物过渡具有进化意义的区域周围,存在超过4米的潮差,这凸显了潮汐动力学作为这些进化过程驱动力的可能重要性。