Short-term coral bleaching is not recorded by skeletal boron isotopes.

Coral skeletal boron isotopes have been established as a proxy for seawater pH, yet it remains unclear if and how this proxy is affected by seawater temperature. Specifically, it has never been directly tested whether coral bleaching caused by high water temperatures influences coral boron isotopes....

Full description

Bibliographic Details
Main Authors: Verena Schoepf, Malcolm T McCulloch, Mark E Warner, Stephen J Levas, Yohei Matsui, Matthew D Aschaffenburg, Andréa G Grottoli
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2014-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4232377?pdf=render
_version_ 1818286563658825728
author Verena Schoepf
Malcolm T McCulloch
Mark E Warner
Stephen J Levas
Yohei Matsui
Matthew D Aschaffenburg
Andréa G Grottoli
author_facet Verena Schoepf
Malcolm T McCulloch
Mark E Warner
Stephen J Levas
Yohei Matsui
Matthew D Aschaffenburg
Andréa G Grottoli
author_sort Verena Schoepf
collection DOAJ
description Coral skeletal boron isotopes have been established as a proxy for seawater pH, yet it remains unclear if and how this proxy is affected by seawater temperature. Specifically, it has never been directly tested whether coral bleaching caused by high water temperatures influences coral boron isotopes. Here we report the results from a controlled bleaching experiment conducted on the Caribbean corals Porites divaricata, Porites astreoides, and Orbicella faveolata. Stable boron (δ11B), carbon (δ13C), oxygen (δ18O) isotopes, Sr/Ca, Mg/Ca, U/Ca, and Ba/Ca ratios, as well as chlorophyll a concentrations and calcification rates were measured on coral skeletal material corresponding to the period during and immediately after the elevated temperature treatment and again after 6 weeks of recovery on the reef. We show that under these conditions, coral bleaching did not affect the boron isotopic signature in any coral species tested, despite significant changes in coral physiology. This contradicts published findings from coral cores, where significant decreases in boron isotopes were interpreted as corresponding to times of known mass bleaching events. In contrast, δ13C and δ18O exhibited major enrichment corresponding to decreases in calcification rates associated with bleaching. Sr/Ca of bleached corals did not consistently record the 1.2°C difference in seawater temperature during the bleaching treatment, or alternatively show a consistent increase due to impaired photosynthesis and calcification. Mg/Ca, U/Ca, and Ba/Ca were affected by coral bleaching in some of the coral species, but the observed patterns could not be satisfactorily explained by temperature dependence or changes in coral physiology. This demonstrates that coral boron isotopes do not record short-term bleaching events, and therefore cannot be used as a proxy for past bleaching events. The robustness of coral boron isotopes to changes in coral physiology, however, suggests that reconstruction of seawater pH using boron isotopes should be uncompromised by short-term bleaching events.
first_indexed 2024-12-13T01:26:35Z
format Article
id doaj.art-b1f254edd16c4318bad776395b3a5519
institution Directory Open Access Journal
issn 1932-6203
language English
last_indexed 2024-12-13T01:26:35Z
publishDate 2014-01-01
publisher Public Library of Science (PLoS)
record_format Article
series PLoS ONE
spelling doaj.art-b1f254edd16c4318bad776395b3a55192022-12-22T00:04:07ZengPublic Library of Science (PLoS)PLoS ONE1932-62032014-01-01911e11201110.1371/journal.pone.0112011Short-term coral bleaching is not recorded by skeletal boron isotopes.Verena SchoepfMalcolm T McCullochMark E WarnerStephen J LevasYohei MatsuiMatthew D AschaffenburgAndréa G GrottoliCoral skeletal boron isotopes have been established as a proxy for seawater pH, yet it remains unclear if and how this proxy is affected by seawater temperature. Specifically, it has never been directly tested whether coral bleaching caused by high water temperatures influences coral boron isotopes. Here we report the results from a controlled bleaching experiment conducted on the Caribbean corals Porites divaricata, Porites astreoides, and Orbicella faveolata. Stable boron (δ11B), carbon (δ13C), oxygen (δ18O) isotopes, Sr/Ca, Mg/Ca, U/Ca, and Ba/Ca ratios, as well as chlorophyll a concentrations and calcification rates were measured on coral skeletal material corresponding to the period during and immediately after the elevated temperature treatment and again after 6 weeks of recovery on the reef. We show that under these conditions, coral bleaching did not affect the boron isotopic signature in any coral species tested, despite significant changes in coral physiology. This contradicts published findings from coral cores, where significant decreases in boron isotopes were interpreted as corresponding to times of known mass bleaching events. In contrast, δ13C and δ18O exhibited major enrichment corresponding to decreases in calcification rates associated with bleaching. Sr/Ca of bleached corals did not consistently record the 1.2°C difference in seawater temperature during the bleaching treatment, or alternatively show a consistent increase due to impaired photosynthesis and calcification. Mg/Ca, U/Ca, and Ba/Ca were affected by coral bleaching in some of the coral species, but the observed patterns could not be satisfactorily explained by temperature dependence or changes in coral physiology. This demonstrates that coral boron isotopes do not record short-term bleaching events, and therefore cannot be used as a proxy for past bleaching events. The robustness of coral boron isotopes to changes in coral physiology, however, suggests that reconstruction of seawater pH using boron isotopes should be uncompromised by short-term bleaching events.http://europepmc.org/articles/PMC4232377?pdf=render
spellingShingle Verena Schoepf
Malcolm T McCulloch
Mark E Warner
Stephen J Levas
Yohei Matsui
Matthew D Aschaffenburg
Andréa G Grottoli
Short-term coral bleaching is not recorded by skeletal boron isotopes.
PLoS ONE
title Short-term coral bleaching is not recorded by skeletal boron isotopes.
title_full Short-term coral bleaching is not recorded by skeletal boron isotopes.
title_fullStr Short-term coral bleaching is not recorded by skeletal boron isotopes.
title_full_unstemmed Short-term coral bleaching is not recorded by skeletal boron isotopes.
title_short Short-term coral bleaching is not recorded by skeletal boron isotopes.
title_sort short term coral bleaching is not recorded by skeletal boron isotopes
url http://europepmc.org/articles/PMC4232377?pdf=render
work_keys_str_mv AT verenaschoepf shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT malcolmtmcculloch shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT markewarner shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT stephenjlevas shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT yoheimatsui shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT matthewdaschaffenburg shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes
AT andreaggrottoli shorttermcoralbleachingisnotrecordedbyskeletalboronisotopes