Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, 54-1514 MIT, Cambridge, MA, 02139, USA.
IFISC (CSIC-UIB), Institute for Cross-Disciplinary Physics and Complex Systems, Palma de Mallorca, Spain.
Nat Commun. 2023 Sep 29;14(1):6092. doi: 10.1038/s41467-023-41469-2.
Marine plankton play a crucial role in carbon storage, global climate, and ecosystem function. Planktonic ecosystems are embedded in patches of water that are continuously moving, stretching, and diluting. These processes drive inhomegeneities on a range of scales, with implications for the integrated ecosystem properties, but are hard to characterize. We present a theoretical framework that accounts for all these aspects; tracking the water patch hosting a drifting ecosystem along with its physical, environmental, and biochemical features. The theory resolves patch dilution and internal physical mixing as a function of oceanic strain and diffusion. Ecological dynamics are parameterized by an idealized nutrient and phytoplankton population and we specifically capture the time evolution of the biochemical spatial variances to represent within-patch heterogeneity. We find that, depending only on the physical processes to which the water patch is subjected, the plankton biomass response to a resource perturbation can vary in size up to six times. This work indicates that we must account for these processes when interpreting and modeling marine ecosystems and provides a framework with which to do so.
海洋浮游生物在碳储存、全球气候和生态系统功能方面发挥着至关重要的作用。浮游生物生态系统嵌入在不断移动、拉伸和稀释的水块中。这些过程在一系列尺度上产生了非均质性,对综合生态系统特性有影响,但难以描述。我们提出了一个理论框架,考虑了所有这些方面;跟踪承载漂流生态系统的水块及其物理、环境和生化特征。该理论将斑块稀释和内部物理混合解析为海洋应变和扩散的函数。生态动力学由理想化的营养物和浮游植物种群参数化,我们特别捕捉生化空间方差的时间演化,以代表斑块内的异质性。我们发现,仅取决于水块所经历的物理过程,浮游生物生物量对资源扰动的响应大小可以变化 6 倍。这项工作表明,我们在解释和模拟海洋生态系统时必须考虑这些过程,并提供了一种这样做的框架。