Centre for Geometric Biology, School of Biological Sciences Monash University, Melbourne, Victoria, Australia.
Department of Biological Science, Florida State University, Tallahassee, FL, USA.
Nat Ecol Evol. 2020 Sep;4(9):1196-1203. doi: 10.1038/s41559-020-1238-y. Epub 2020 Jul 6.
The distance travelled by marine larvae varies by seven orders of magnitude. Dispersal shapes marine biodiversity, and must be understood if marine systems are to be well managed. Because warmer temperatures quicken larval development, larval durations might be systematically shorter in the tropics relative to those at high latitudes. Nevertheless, life history and hydrodynamics also covary with latitude-these also affect dispersal, precluding any clear expectation of how dispersal changes at a global scale. Here we combine data from the literature encompassing >750 marine organisms from seven phyla with oceanographic data on current speeds, to quantify the overall latitudinal gradient in larval dispersal distance. We find that planktonic duration increased with latitude, confirming predictions that temperature effects outweigh all others across global scales. However, while tropical species have the shortest planktonic durations, realized dispersal distances were predicted to be greatest in the tropics and at high latitudes, and lowest at mid-latitudes. At high latitudes, greater dispersal distances were driven by moderate current speed and longer planktonic durations. In the tropics, fast currents overwhelmed the effect of short planktonic durations. Our results contradict previous hypotheses based on biology or physics alone; rather, biology and physics together shape marine dispersal patterns.
海洋幼虫的移动距离变化幅度可达七个数量级。扩散塑造了海洋生物多样性,如果要对海洋系统进行良好的管理,就必须了解扩散。由于较高的温度会加速幼虫的发育,因此与高纬度地区相比,幼虫的持续时间可能在热带地区更短。然而,生活史和水动力也与纬度相关——这些因素也会影响扩散,从而使任何关于全球扩散变化的明确预期都变得不可能。在这里,我们结合了来自文献的数据,这些数据涵盖了来自七个门的 750 多种海洋生物,以及有关海流速度的海洋学数据,以量化幼虫扩散距离的总体纬度梯度。我们发现浮游期随着纬度的增加而增加,证实了在全球范围内,温度的影响大于其他所有因素的预测。然而,虽然热带物种的浮游期最短,但在热带和高纬度地区,实际的扩散距离预计最大,而在中纬度地区则最小。在高纬度地区,更大的扩散距离是由中等的海流速度和较长的浮游期驱动的。在热带地区,快速的海流削弱了浮游期短的影响。我们的研究结果与仅基于生物学或物理学的先前假设相矛盾;相反,生物学和物理学共同塑造了海洋扩散模式。