Seawater carbonate chemistry and shell microstructure, mechanical properties of an edible estuarine oyster

Ocean acidification (OA) is well-known for impairing marine calcification; however, the end response of several essential species to this perturbation remains unknown. Decreased pH and saturation levels (Omega) of minerals under OA is projected to alter shell crystallography and thus to reduce shell...

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Bibliographic Details
Main Authors: Meng, Yuan, Guo, Zhenbin, Yao, Haimin, Yeung, Kelvin W K, Thiyagarajan, Vengatesen
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
EXP
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.908459
https://doi.org/10.1594/PANGAEA.908459
Description
Summary:Ocean acidification (OA) is well-known for impairing marine calcification; however, the end response of several essential species to this perturbation remains unknown. Decreased pH and saturation levels (Omega) of minerals under OA is projected to alter shell crystallography and thus to reduce shell mechanical properties. This study examined this hypothesis using a commercially important estuarine oyster Magallana hongkongensis. Although shell damage occurred on the outmost prismatic layer and the undying myostracum at decreased pH 7.6 and 7.3, the major foliated layer was relatively unharmed. Oysters maintained their shell hardness and stiffness through altered crystal unit orientation under pH 7.6 conditions. However, under the undersaturated conditions (Omega Cal ~ 0.8) at pH 7.3, the realigned crystal units in foliated layer ultimately resulted in less stiff shells which indicated although estuarine oysters are mechanically resistant to unfavorable calcification conditions, extremely low pH condition is still a threat to this essential species.