Japan Geoscience Union Meeting 2018

Presentation information

[EE] Oral

B (Biogeosciences) » B-PT Paleontology

[B-PT04] Biomineralization and the Geochemistry of Proxies

Sun. May 20, 2018 1:45 PM - 3:15 PM 101 (1F International Conference Hall, Makuhari Messe)

convener:Takashi Toyofuku(Japan Agency for Marine-Earth Science and Technology (JAMSTEC)), Hiroshi Kitazato(Tokyo University of Marine Science and Technology (TUMSAT)), Jelle Bijma(アルフレッドウェゲナー極域海洋研究所, 共同), Kotaro Hirose(Faculty of Science & Engineering, Waseda University), Chairperson:Bijma Jelle(AWI), Toyofuku Takashi

2:15 PM - 2:30 PM

[BPT04-03] Transgenerational exposure of the Manila clam Ruditapes philippinarum to ocean acidification: Preferential uptake of metabolic carbon facilitates shell formation

*Liqiang ZHAO1, Stefania Milano2, Eric O. Walliser2, Bernd R. Schone2 (1.Atmosphere and Ocean Research Institute, The University of Tokyo, 2.Institute of Geosciences, University of Mainz)

Keywords:Ocean acidification, Acclimation and adaption, Marine bivalves

Ocean acidification profoundly affects marine bivalves, and consequently, understanding their capacity for acclimation and adaption to lower pH over multiple generations is crucial to make predictions about the fate of this economically and ecologically important fauna in an acidifying ocean. Transgenerational exposure to an acidification scenario projected by the end of the century (i.e., pH 7.7) has been shown to confer resilience to juvenile offspring of the Manila clam (Ruditapes philippinarum). However, whether and to what extent this resilience can persist into adulthood are largely unknown and the mechanisms driving transgenerational acclimation remain poorly understood. Here, we take observations of aforementioned juvenile clams further into adulthood and observe similar transgenerational responses. Under acidified conditions, clams originating from parents reproductively exposed to the same level of low pH show a significantly faster shell growth rate, a higher condition index and a lower standard metabolic rate compared to those without prior history of transgenerational acclimation. Further analyses of stable carbon isotopic signatures in dissolved inorganic carbon of seawater, individual soft tissues and shells reveal that up to 61 % of shell carbonate comes from metabolically generated carbon, suggesting that transgenerationally acclimated clams can preferentially extract internal metabolic carbon rather than actively transport external seawater inorganic carbon to construct their shells, the latter known to be energetically expensive. Noteworthily, while a large metabolic carbon contribution (45 %) is seen in non-acclimated clams, a significant reduction in the rate of shell growth indicates it might occur at the expense of other calcification-relevant processes. It therefore seems plausible that R. philippinarum implements a less costly and more efficient energy-utilizing strategy to mitigate the impact of acidified seawater following transgenerational acclimation. Collectively, our findings indicate that marine bivalves are likely more resilient to ocean acidification projected for the end of the century than previously thought.