Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress

The Florida Keys reef tract (FKRT) has a unique geological history wherein Holocene sea-level rise and bathymetry interacted, resulting in a reef-building system with notable spatial differences in reef development. Overprinted on this geologic history, recent global and local stressors have led to...

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Main Authors: Elizabeth Ann Lenz, Lucy A. Bartlett, Anastasios Stathakopoulos, Ilsa B. Kuffner
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-06-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2021.615795/full
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author Elizabeth Ann Lenz
Elizabeth Ann Lenz
Lucy A. Bartlett
Anastasios Stathakopoulos
Ilsa B. Kuffner
author_facet Elizabeth Ann Lenz
Elizabeth Ann Lenz
Lucy A. Bartlett
Anastasios Stathakopoulos
Ilsa B. Kuffner
author_sort Elizabeth Ann Lenz
collection DOAJ
description The Florida Keys reef tract (FKRT) has a unique geological history wherein Holocene sea-level rise and bathymetry interacted, resulting in a reef-building system with notable spatial differences in reef development. Overprinted on this geologic history, recent global and local stressors have led to degraded reefs dominated by fleshy algae, soft corals, and sponges. Here, we assessed how coral physiology (calcification rate, tissue thickness, reproduction, symbiosis, and bleaching) varies seasonally (winter vs. summer) and geographically using 40 colonies of the mustard hill coral Porites astreoides from four sites across 350 km along the FKRT from 2015 to 2017. The study coincided with a high-temperature event in late summer 2015 that caused heterogeneous levels of coral bleaching across sites. Bleaching severity differed by site, with bleaching response more aligned with heat stress retroactively calculated from local degree heating weeks than those predicted by satellites. Despite differences in temperature profiles and bleaching severity, all colonies hosted Symbiodiniaceae of the same genus (formerly Clade A and subtypes). Overall, P. astreoides at Dry Tortugas National Park, the consistently coolest site, had the highest calcification rates, symbiont cell densities, and reproductive potential (all colonies were reproductive, with most planula larvae per polyp). Corals at Dry Tortugas and Fowey Rocks Light demonstrated strong seasonality in net calcification (higher in summer) and did not express visual or partial-mortality responses from the bleaching event; in contrast, colonies in the middle and southern part of the upper keys, Sombrero Key and Crocker Reef, demonstrated similar reduced fitness from bleaching, but differential recovery trajectories following the heat stress. Identifying reefs, such as Dry Tortugas and possibly Fowey Rocks Light that may serve as heat-stress refugia, is important in selecting candidate sites for adaptive reef-management strategies, such as selective propagation and assisted gene flow, to increase coral-species adaptation to ocean warming.
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spelling doaj.art-a538dfe476b44a308384bc71894a1daa2022-12-21T20:32:50ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452021-06-01810.3389/fmars.2021.615795615795Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature StressElizabeth Ann Lenz0Elizabeth Ann Lenz1Lucy A. Bartlett2Anastasios Stathakopoulos3Ilsa B. Kuffner4Hawai‘i Institute of Marine Biology, Kāne‘ohe, HI, United StatesUniversity of Hawai‘i Sea Grant College Program, University of Hawai‘i at Mānoa, Honolulu, HI, United StatesU.S. Geological Survey, St. Petersburg Coastal and Marine Science Center, St. Petersburg, FL, United StatesU.S. Geological Survey, St. Petersburg Coastal and Marine Science Center, St. Petersburg, FL, United StatesU.S. Geological Survey, St. Petersburg Coastal and Marine Science Center, St. Petersburg, FL, United StatesThe Florida Keys reef tract (FKRT) has a unique geological history wherein Holocene sea-level rise and bathymetry interacted, resulting in a reef-building system with notable spatial differences in reef development. Overprinted on this geologic history, recent global and local stressors have led to degraded reefs dominated by fleshy algae, soft corals, and sponges. Here, we assessed how coral physiology (calcification rate, tissue thickness, reproduction, symbiosis, and bleaching) varies seasonally (winter vs. summer) and geographically using 40 colonies of the mustard hill coral Porites astreoides from four sites across 350 km along the FKRT from 2015 to 2017. The study coincided with a high-temperature event in late summer 2015 that caused heterogeneous levels of coral bleaching across sites. Bleaching severity differed by site, with bleaching response more aligned with heat stress retroactively calculated from local degree heating weeks than those predicted by satellites. Despite differences in temperature profiles and bleaching severity, all colonies hosted Symbiodiniaceae of the same genus (formerly Clade A and subtypes). Overall, P. astreoides at Dry Tortugas National Park, the consistently coolest site, had the highest calcification rates, symbiont cell densities, and reproductive potential (all colonies were reproductive, with most planula larvae per polyp). Corals at Dry Tortugas and Fowey Rocks Light demonstrated strong seasonality in net calcification (higher in summer) and did not express visual or partial-mortality responses from the bleaching event; in contrast, colonies in the middle and southern part of the upper keys, Sombrero Key and Crocker Reef, demonstrated similar reduced fitness from bleaching, but differential recovery trajectories following the heat stress. Identifying reefs, such as Dry Tortugas and possibly Fowey Rocks Light that may serve as heat-stress refugia, is important in selecting candidate sites for adaptive reef-management strategies, such as selective propagation and assisted gene flow, to increase coral-species adaptation to ocean warming.https://www.frontiersin.org/articles/10.3389/fmars.2021.615795/fullscleractiniain situ calcification ratesreproductioncoral-algal symbiosiscoral reef degradationbuoyant weight
spellingShingle Elizabeth Ann Lenz
Elizabeth Ann Lenz
Lucy A. Bartlett
Anastasios Stathakopoulos
Ilsa B. Kuffner
Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
Frontiers in Marine Science
scleractinia
in situ calcification rates
reproduction
coral-algal symbiosis
coral reef degradation
buoyant weight
title Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
title_full Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
title_fullStr Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
title_full_unstemmed Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
title_short Physiological Differences in Bleaching Response of the Coral Porites astreoides Along the Florida Keys Reef Tract During High-Temperature Stress
title_sort physiological differences in bleaching response of the coral porites astreoides along the florida keys reef tract during high temperature stress
topic scleractinia
in situ calcification rates
reproduction
coral-algal symbiosis
coral reef degradation
buoyant weight
url https://www.frontiersin.org/articles/10.3389/fmars.2021.615795/full
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