Abstract

Climate-driven shifts of coastal species’ ranges constitute a key factor shaping both the vegetation composition and biodiversity of coastal ecosystems. Although phylogeographic studies relying on genetic data have shed light on the evolutionary history of macroalgae along the Northwest Pacific (NW-Pacific) coast, their distribution dynamics are less understood and require interdisciplinary examination. Here, we used a combination of species distribution models (SDMs) and genetic data to explain the causes of population persistence and genetic differentiation and their consequences for the brown seaweed Sargassum horneri in the NW-Pacific. In this region, the phylogeographic structure of S. horneri was analyzed by screening 72 populations spawning across the entire coastal distribution and obtaining their mtDNA cox3 data. Population genetic structure and SDMs based on paleoclimatic data consistently revealed that southern coasts of the Sea of Japan, North-Pacific-Japan, and the northern part of Okinawa Trough might have served as potential refugia for S. horneri during the Last Glacial Maximum (LGM). Furthermore, we projected the distribution dynamics of S. horneri under future climate scenarios. The range of S. horneri was predicted to move northward, with a significant loss of suitable habitat, under the high emissions scenario (RCP 8.5). By contrast, projected range shifts were minimal under the low emissions scenario (RCP 2.6). Furthermore, North-Pacific-Japan was projected to be long-term persistence habitat for S. horneri under future climatic conditions, thus including this area in conservation planning could help mitigate for climate change implications. Our results enable a better understanding of the impacts of climate change on the spatio-temporal distribution of macroalgae and how this can inform coastal management and marine conservation planning.

Highlights

  • Understanding the impacts of global warming on seaweed communities is a central challenge for marine species conservation

  • Lineage I dominated the populations from the North-Pacific-Japan; Lineage II dominated coasts of Pacific-Japan and Korea; Lineage III occurred in the populations from South-Pacific-Japan, China, Korea, and Sea of Japan (Supplementary Table S1, Figures 1A,B)

  • Genetic divergence was detected in S. horneri populations along the coasts of NWPacific, suggesting multiple ancient refugia (e.g., North-PacificJapan, South Sea of Japan, and northern Okinawa Trough)

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Summary

Introduction

Understanding the impacts of global warming on seaweed communities is a central challenge for marine species conservation. Canopy-forming seaweed has experienced noticeable regression because of climatic changes and anthropogenic activities (Casado-Amezúa et al, 2019). Canopy-forming species, such as large brown seaweeds support elevated levels of biodiversity through their complex structure (holdfast and surrounding substratum), the regression has negatively affected these associated marine species (Verdura et al, 2018; Sudo et al, 2020). Pessarrodona et al (2019) investigated how climatic-driven substitutions of two foundation species, Laminaria hyperborea (cold-affinity) and L. ochroleuca (warm-affinity), influenced community, trophic structure and functioning through processes associated with the cycling of organic matter (including biomass production, detritus flow, herbivory, and decomposition)

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