4.7 Article

Quantifying the dynamics of rocky intertidal sessile communities along the Pacific coast of Japan: implications for ecological resilience

Journal

SCIENTIFIC REPORTS
Volume 11, Issue 1, Pages -

Publisher

NATURE PORTFOLIO
DOI: 10.1038/s41598-021-95348-1

Keywords

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Funding

  1. Cooperative Program of the Atmosphere and Ocean Research Institute, The University of Tokyo [108, 104, 107, 101, 103]
  2. Japan Society for the Promotion of Science KAKENHI [20570012, 24570012, 5K07208, 18H02503]
  3. Tohoku Ecosystem-Associated Marine Sciences (TEAMS) project
  4. Grants-in-Aid for Scientific Research [18H02503, 24570012] Funding Source: KAKEN

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Long-term patterns in community trajectories provide insights into ecological resilience, but require extensive census data. The stable trajectory was most common, with varying features and recovery rates among regions, while trajectories and temporal invariabilities also differed among regions seemingly linked to ocean current fluctuations.
Long-term patterns in trajectories of natural communities provide insights into ecological resilience, but their assessment requires long-term census data. We analyzed 16-year census data for intertidal communities from 30 rocky shores along Japan's Pacific coast to assign community change to four possible trajectories (stable, reversible, abrupt, or linear) representing different aspects of ecological resilience, and to estimate multiple metrics of temporal invariability (species richness, species composition, and community abundance). We examined (1) how the prevalence of the four trajectories differs among regions, (2) how the features (model coefficients) of each trajectory vary among regions, and (3) how the temporal invariabilities differ among trajectories and regions. We found that the stable trajectory was the most common. Its features differed among regions, with a faster recovery to steady-state equilibrium in low-latitude regions. Furthermore, trajectories and temporal invariabilities both varied among regions, seemingly in association with the strength of ocean current fluctuations. Thus, the relationship between community temporal invariability and trajectory may be weak or absent, at least at the regional scale.

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