Abstract

Globally, species are migrating in an attempt to track optimal isotherms as climate change increasingly warms existing habitats. Stony corals are severely threatened by anthropogenic warming, which has resulted in repeated mass bleaching and mortality events. Since corals are sessile as adults and with a relatively old age of sexual maturity, they are slow to latitudinally migrate, but corals may also migrate vertically to deeper, cooler reefs. Herein we describe vertical migration of the Mediterranean coral Oculina patagonica from less than 10 m depth to > 30 m. We suggest that this range shift is a response to rapidly warming sea surface temperatures on the Israeli Mediterranean coastline. In contrast to the vast latitudinal distance required to track temperature change, this species has migrated deeper where summer water temperatures are up to 2 °C cooler. Comparisons of physiology, morphology, trophic position, symbiont type, and photochemistry between deep and shallow conspecifics revealed only a few depth-specific differences. At this study site, shallow colonies typically inhabit low light environments (caves, crevices) and have a facultative relationship with photosymbionts. We suggest that this existing phenotype aided colonization of the mesophotic zone. This observation highlights the potential for other marine species to vertically migrate.

Highlights

  • Species are migrating in an attempt to track optimal isotherms as climate change increasingly warms existing habitats

  • Surveys conducted along the Israeli coasts by the Morris Kahn Marine Research Station Long Term Ecological Research program (MKMRS LTER; established in 2014—https://med-lter.haifa.ac.il/index.php/en/data-base) recently reported the presence of O. patagonica much deeper than usual, at 30 m depth (Ashdod, Israel, autumn 2019)

  • The origin of these colonies remains to be proven, O. patagonica is increasing in abundance at mesophotic depths

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Summary

Introduction

Species are migrating in an attempt to track optimal isotherms as climate change increasingly warms existing habitats. We suggest that increasing sea surface temperature over the last three decades in the eastern Mediterranean (> 3 °C)[36] has breached the upper thermal threshold of O. patagonica, and concomitant with warming in deeper waters has drawn this species to seek refuge in the cooler, deeper waters along the Israeli coast (1–2 °C cooler in the summer, Fig. 1C). These colonies may have been present yet undetected at deeper sites before 2019, mesophotic O. patagonica has never been reported in the ­literature[14,32,33]

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