Fig. 1. Predicting the future using a technique to measure the shell density of shellfish larvae.
Calcifying organisms
Organisms that form hard tissues, such as calcified skeletons or shells, using free carbonate ions (CO32-) and calcium ions (Ca2+) found in seawater.
Microfocus X-ray computed tomography (MXCT)
An imaging technique capable of revealing detailed three-dimensional information about both the surface and internal structure of microscopic objects following irradiation with X-rays from all directions and capturing of X-ray images, which are then reconstructed by a computer.
As global warming intensifies, so does ocean acidification. Such ocean acidification poses a serious threat to marine ecosystems. It not only lowers the pH of seawater but also reduces the “aragonite saturation state (Ωaragonaite)※3, ※4 ”. Aragonite is a crystalline form of calcium carbonate. When the “aragonite saturation state” is 1 or higher, it indicates a supersaturated state; conversely, values below 1 indicate an unsaturated state. The value is as an indicator of how easily organisms can form aragonite-based shells or skeletons. When the aragonite saturation state decreases, it is more difficult for organisms to form aragonite shells or skeletons. However, evaluating the effects of ocean acidification on early developmental stages of organisms such as plankton and mollusk larvae with aragonite shells, has proven challenging. Their shells are exceptionally small (approximately 0.1 mm in diameter and only a few micrometers※5 thick), which makes precise quantitative assessment more challenging than with mature specimens.
To address the challenges above, Keisuke Shimizu (Associate Researcher) and Katsunori Kimoto (Acting Group Leader) from the Japan Agency for Marine-Earth Science and Technology Research Institute for Global Change Earth Surface System Research Center, alongside Masahide Wakita (Associate Researcher, Mutsu Research Institute), carried out joint research with Takenori Sasaki (Associate Professor, University Museum at the University of Tokyo). The team analyzed the morphology of the shells of shellfish larvae, using high-resolution MXCT and scanning electron microscopy (SEM)※6, as well as gene expression. Globally, the research team is the first to successfully visualize and quantify the effects of decreased aragonite saturation on the growth and structure of extremely small shells (approximately 0.1 mm) composed of aragonite crystals, using shell density (which is analogous to human bone density) as a novel growth marker. In addition, the findings suggest that a decrease in aragonite saturation may both directly impact shells and influence gene expression domains involved in shell formation in shellfish larvae. The findings could facilitate prediction of the effects of environmental change (such as global warming and acidification) on calcifying organisms such as shellfish and corals.
These results have been published in the Journal of Molluscan Studies on September 18 (Japan time). The research was conducted with the support of a Grant-in-Aid for Scientific Research from the Japan Society for the Promotion of Science (KAKENHI; JP23H02299).
Keisuke Shimizu1, Katsunori Kimoto1, Masahide Wakita1, Takenori Sasaki2
Aragonite
Calcium carbonate (CaCO3) exists in three forms, with distinct crystal structures: aragonite, calcite, and vaterite. The shells of mollusk larvae are made up of aragonite, whereas the shells of mature mollusks contain either aragonite or calcite—the type of calcium carbonate crystal varies by species.
Aragonite saturation state (Ωaragonaite)
A value indicating the level of saturation of aragonite in seawater. When the “aragonite saturation state” is ≥ 1, it indicates a supersaturated state; conversely, values < 1 indicate an unsaturated state. Therefore, the higher the value, the more easily organisms can form calcium carbonate (aragonite) shells; conversely, the lower the value, the more difficult shell formation becomes. Ωaragonaite is an indicator of the degree of ocean acidification, separate from pH.
Micrometer (µm)
A unit of length equal to one-thousandth of a millimeter (mm).
Scanning electron microscope (SEM)
A microscope that uses signals obtained by directing an electron beam at the surface of a sample to observe microscopic structures at the nanometer (one-millionth of a millimeter) scale in three dimension.
For this study
Keisuke Shimizu, Researcher, Research Institute for Global Change(RIGC), Earth Surface System Research Center(ESS), Marine Ecosystem Research Group, JAMSTEC
For press release