Abstract

Widespread mortality of intertidal biota was observed following the 7.8 Mw Kaikōura earthquake in November 2016. To understand drivers of change and recovery in nearshore ecosystems, we quantified the variation in relative sea-level changes caused by tectonic uplift and evaluated their relationships with ecological impacts with a view to establishing the minimum threshold and overall extent of the major effects on rocky shores. Vertical displacement of contiguous 50 m shoreline sections was assessed using comparable LiDAR data to address initial and potential ongoing change across a 100 km study area. Co-seismic uplift accounted for the majority of relative sea-level change at most locations. Only small changes were detected beyond the initial earthquake event, but they included the weathering of reef platforms and accumulation of mobile gravels that continue to shape the coast. Intertidal vegetation losses were evident in equivalent intertidal zones at all uplifted sites despite considerable variation in the vertical displacement they experienced. Nine of ten uplifted sites suffered severe (>80%) loss in habitat-forming algae and included the lowest uplift values (0.6 m). These results show a functional threshold of c.1/4 of the tidal range above which major impacts were sustained. Evidently, compensatory recovery has not occurred—but more notably, previously subtidal algae that were uplifted into the low intertidal zone where they ought to persist (but did not) suggests additional post-disturbance adversities that have contributed to the overall effect. Continuing research will investigate differences in recovery trajectories across the affected area to identify factors and processes that will lead to the regeneration of ecosystems and resources.

Highlights

  • Relative sea-level trends are pervasive drivers of change in nearshore coastal systems due to the multitude of social and ecological relationships that are structured by the position of land in relation to the sea [1]

  • This work has been an important milestone in relating ecological damage along an extensive stretch of coastline to vertical displacement caused by one of the major seismic events in modern times

  • This is the first study to quantify relative sea-level changes at the position of the new intertidal environment and the first to estimate the extent of earthquake impacts on major habitat-forming algal species that are characteristic of the Kaikōura region

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Summary

Introduction

Relative sea-level trends are pervasive drivers of change in nearshore coastal systems due to the multitude of social and ecological relationships that are structured by the position of land in relation to the sea [1]. Enduring sea-level changes present a specific set of challenges that differ from those associated with periodic extreme events. They are more likely to force long-term adjustments to the spatial configuration of coastal landscapes upon which both periodic extreme events and regular hydrological fluctuations interact [2]. Rapid changes in relative sea-levels can result in widespread disturbance to the antecedent pattern of development in both natural and anthropogenic environments. While various degrees of resistance or resilience to these changes are a feature of social–ecological systems, there are tipping points beyond which major losses are sustained [8,9,10]

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