Graham Jeffrey B, Lee Heather J
Center for Marine Biotechnology and Biomedicine and Marine Biology Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, 92093-0204, USA.
Physiol Biochem Zool. 2004 Sep-Oct;77(5):720-31. doi: 10.1086/425184.
The air-breathing fishes have heuristic importance as possible models for the Paleozoic evolution of vertebrate air breathing and the transition to land. A recent hypothesis about this transition suggests that the diverse assemblage of marine amphibious fishes occurring primarily in tropical, high intertidal zone habitats are analogs of early tetrapods and that the intertidal zone, not tropical freshwater lowlands, was the springboard habitat for the Devonian land transition by vertebrates. Here we argue that selection pressures imposed by life in the intertidal zone are insufficient to have resulted in the requisite aerial respiratory capacity or the degree of separation from water required for the vertebrate land transition. The extant marine amphibious fishes, which occur mainly on rocky shores or mudflats, have reached the limit of their niche expansion onto land and remain tied to water by respiratory structures that are less efficient in air and more vulnerable to desiccation than lungs. We further argue that evolutionary contingencies actuated by the Devonian origin of the tetrapods marked a critical point of divergence for a way of life in which selection pressures would operate on the physiology, morphology, and natural history of the different vertebrate groups. While chronically hypoxic and shallow water conditions in the habitats of some primitive bony fishes and some amphibians appear similar to the conditions that prevailed in the Devonian, markedly different selection pressures have operated on other amphibians and bony fishes over the 300 million years since the vertebrate land transition. For example, both egg development and larval metamorphosis in extant amphibians are geared mainly toward compensating for the uncertainty of habitat water quality or even the absence of water by minimizing the time required to develop there. In contrast, reproduction by most intertidal (and amphibious) fishes, all of which are teleosts, remains dependent on a planktonic larval phase and is characterized by specializations (brooding) that minimize overdispersal and maximize recruitment back to the littoral habitat.
作为脊椎动物空气呼吸的古生代演化及向陆地过渡的可能模型,用肺呼吸的鱼类具有启发意义。关于这一过渡的一个最新假说是,主要出现在热带高潮间带栖息地的各种海洋两栖鱼类是早期四足动物的类似物,并且潮间带而非热带淡水低地是泥盆纪脊椎动物向陆地过渡的跳板栖息地。在此我们认为,潮间带生活所施加的选择压力不足以产生脊椎动物向陆地过渡所需的空中呼吸能力或与水的分离程度。现存的海洋两栖鱼类主要出现在岩石海岸或泥滩,它们在向陆地的生态位扩张方面已达到极限,并且由于其呼吸结构在空气中效率较低且比肺更容易受到干燥影响,因而仍然与水紧密相连。我们还认为,四足动物在泥盆纪起源所引发的进化偶然性标志着一种生活方式的关键分歧点,在这种生活方式中,选择压力将作用于不同脊椎动物类群的生理、形态和自然史。虽然一些原始硬骨鱼类和一些两栖动物栖息地的长期缺氧和浅水条件似乎与泥盆纪时盛行的条件相似,但自脊椎动物向陆地过渡以来的3亿年里,其他两栖动物和硬骨鱼类受到了明显不同的选择压力。例如,现存两栖动物的卵发育和幼体变态主要是为了通过尽量缩短在那里发育所需的时间来补偿栖息地水质的不确定性甚至水的缺失。相比之下,大多数潮间带(和两栖)鱼类(均为硬骨鱼)的繁殖仍然依赖浮游幼体阶段,其特点是具有一些特化(育雏),可尽量减少过度扩散并使回到沿岸栖息地的补充量最大化。