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. 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.
School of Earth and Environment, The University of Western Australia and ARC Centre of Excellence for Coral Reef Studies, Crawley, WA, Australia; School of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America.
Verena
V
Schoepf
School of Earth and Environment, The University of Western Australia and ARC Centre of Excellence for Coral Reef Studies, Crawley, WA, Australia.
Malcolm T
MT
McCulloch
School of Marine Science and Policy, University of Delaware, Lewes, Delaware, United States of America.
Mark E
ME
Warner
School of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America.
Stephen J
SJ
Levas
School of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America.
Yohei
Y
Matsui
School of Marine Science and Policy, University of Delaware, Lewes, Delaware, United States of America.
Matthew D
MD
Aschaffenburg
School of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America.
Andréa G
AG
Grottoli
D000704:Analysis of Variance; D000818:Animals; D037421:Anthozoa / Q000502:physiology*; D001842:Bone and Bones / Q000378:metabolism*; D001895:Boron / Q000378:metabolism*; D002113:Calcification, Physiologic; D002247:Carbon Isotopes; D002734:Chlorophyll / Q000378:metabolism; D000077194:Chlorophyll A; D007554:Isotopes; D010103:Oxygen Isotopes; D013997:Time Factors; D014131:Trace Elements
D002247:Carbon Isotopes; D007554:Isotopes; D010103:Oxygen Isotopes; D014131:Trace Elements; D002734:Chlorophyll; D001895:Boron; D000077194:Chlorophyll A