Assessment of paleo-ocean pH records from boron isotope ratio in the Pacific and Atlantic ocean corals: Role of anthropogenic CO<sub>2</sub> forcing and oceanographic factors to pH variability

Abstract

<p><strong>Abstract.</strong> Boron isotopes (δ<sup>11</sup>B) records from tropical ocean corals have been used to reconstruct paleo-pH of ocean for the past several decades to few centuries which are comparable to the resolution of instrumental records. In most of the studies, attempts have been made to decipher the role of anthropogenic CO<sub>2</sub> forcing to recent trend of ocean acidification based on δ<sup>11</sup>B derived paleo-pH records. However, such attempts in past were often hindered by limited knowledge of oceanographic factors that contributed to past pH variability and changes. In this study, we have evaluated pH records reconstructed using δ<sup>11</sup>B records from the Pacific and the Atlantic Oceans corals and investigated major forcing factors that contributed to sub annual-decadal scale pH variability and changes since the industrial era ~<span class="thinspace"></span>1850<span class="thinspace"></span>AD.</p> <p>To the best of our knowledge, total eight δ<sup>11</sup>B records from the Pacific and two from the Atlantic Oceans are available in published literatures. The compilations of these records show large variability; range between 26.27–20.82<span class="thinspace"></span>‰ which corresponds to pH range 8.40–7.63 respectively. Our investigation of pH records from the Pacific ocean based on principal component analysis (PCA) reveals that atmospheric CO<sub>2</sub> can explains maximum up to ~<span class="thinspace"></span>26<span class="thinspace"></span>% of the total pH variability during 1950–2004<span class="thinspace"></span>AD, followed by the ocean-climate oscillations (i.e. ENSO and PDO) driven oceanographic factors up to ~<span class="thinspace"></span>17<span class="thinspace"></span>%. The remaining large variability (~<span class="thinspace"></span>57<span class="thinspace"></span>%) could not be explained by above forcing factors and hence we invoke possible influence of metabolic processes of corals and/or changes in micro-environments within the reefs which are often neglected in interpreting paleo-pH records. Therefore, we highlight the need for detailed investigation in future studies to understand about the exact mechanism, processes/factors that controlled boron isotope fractionations in coral reef environments. Further, our investigation reveals that amplitude of the ENSO driven pH variability shows fivefold increase during 1980–2000<span class="thinspace"></span>AD compared to the previous three decades (1950–1980<span class="thinspace"></span>AD). This observation is consistent with the historical records of global coral bleaching events and therefore underscores role of ENSO driven environmental stress responsible for coral bleaching events. Considering model based projections of increasing frequency and amplitude of extreme ENSO events in the backdrop of recent global warming, bleaching events are likely to increase in the next decades/centuries.</p>