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Ocean Warming Amplifies the Effects of Ocean Acidification on Skeletal Mineralogy and Microstructure in the Asterinid Starfish Aquilonastra yairi. JOURNAL OF MARINE SCIENCE AND ENGINEERING 2022. [DOI: 10.3390/jmse10081065] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/27/2023]
Abstract
Ocean acidification and ocean warming compromise the capacity of calcifying marine organisms to generate and maintain their skeletons. While many marine calcifying organisms precipitate low-Mg calcite or aragonite, the skeleton of echinoderms consists of more soluble Mg-calcite. To assess the impact of exposure to elevated temperature and increased pCO2 on the skeleton of echinoderms, in particular the mineralogy and microstructure, the starfish Aquilonastra yairi (Echinodermata: Asteroidea) was exposed for 90 days to simulated ocean warming (27 °C and 32 °C) and ocean acidification (455 µatm, 1052 µatm, 2066 µatm) conditions. The results indicate that temperature is the major factor controlling the skeletal Mg (Mg/Ca ratio and Mgnorm ratio), but not for skeletal Sr (Sr/Ca ratio and Srnorm ratio) and skeletal Ca (Canorm ratio) in A. yairi. Nevertheless, inter-individual variability in skeletal Sr and Ca ratios increased with higher temperature. Elevated pCO2 did not induce any statistically significant element alterations of the skeleton in all treatments over the incubation time, but increased pCO2 concentrations might possess an indirect effect on skeletal mineral ratio alteration. The influence of increased pCO2 was more relevant than that of increased temperature on skeletal microstructures. pCO2 as a sole stressor caused alterations on stereom structure and degradation on the skeletal structure of A. yairi, whereas temperature did not; however, skeletons exposed to elevated pCO2 and high temperature show a strongly altered skeleton structure compared to ambient temperature. These results indicate that ocean warming might exacerbate the skeletal maintaining mechanisms of the starfish in a high pCO2 environment and could potentially modify the morphology and functions of the starfish skeleton.
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Armstrong EJ, Watson SA, Stillman JH, Calosi P. Elevated temperature and carbon dioxide levels alter growth rates and shell composition in the fluted giant clam, Tridacna squamosa. Sci Rep 2022; 12:11034. [PMID: 35773289 PMCID: PMC9247080 DOI: 10.1038/s41598-022-14503-4] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/29/2022] [Accepted: 06/08/2022] [Indexed: 11/09/2022] Open
Abstract
Giant clams produce massive calcified shells with important biological (e.g., defensive) and ecological (e.g., habitat-forming) properties. Whereas elevated seawater temperature is known to alter giant clam shell structure, no study has examined the effects of a simultaneous increase in seawater temperature and partial pressure of carbon dioxide (pCO2) on shell mineralogical composition in these species. We investigated the effects of 60-days exposure to end-of-the-century projections for seawater temperature (+ 3 °C) and pCO2 (+ 500 µatm) on growth, mineralogy, and organic content of shells and scutes in juvenile Tridacna squamosa giant clams. Elevated temperature had no effect on growth rates or organic content, but did increase shell [24Mg]/[40Ca] as well as [40Ca] in newly-formed scutes. Elevated pCO2 increased shell growth and whole animal mass gain. In addition, we report the first evidence of an effect of elevated pCO2 on element/Ca ratios in giant clam shells, with significantly increased [137Ba]/[40Ca] in newly-formed shells. Simultaneous exposure to both drivers greatly increased inter-individual variation in mineral concentrations and resulted in reduced shell N-content which may signal the onset of physiological stress. Overall, our results indicate a greater influence of pCO2 on shell mineralogy in giant clams than previously recognized.
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Affiliation(s)
- Eric J Armstrong
- Department of Integrative Biology, University of California, 3040 Valley Life Sciences Building #3140, Berkeley, CA, 94720-3140, USA. .,Estuary & Ocean Science Center and Department of Biology, Romberg Tiburon Campus, San Francisco State University, 3150 Paradise Drive, Tiburon, CA, 94920, USA. .,PSL Research University, EPHE, CNRS, Université de Perpignan, Perpignan, France.
| | - Sue-Ann Watson
- Biodiversity and Geosciences Program, Museum of Tropical Queensland, Queensland Museum Network, Townsville, QLD, 4810, Australia.,Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD, 4811, Australia
| | - Jonathon H Stillman
- Department of Integrative Biology, University of California, 3040 Valley Life Sciences Building #3140, Berkeley, CA, 94720-3140, USA.,Estuary & Ocean Science Center and Department of Biology, Romberg Tiburon Campus, San Francisco State University, 3150 Paradise Drive, Tiburon, CA, 94920, USA
| | - Piero Calosi
- Marine Biology & Ecology Research Center, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK.,Département de Biologie, Chimie et Géographie, Université du Québec à Rimouski, 300 Allée Ursulines, Rimouski, QC, G5L 3A1, Canada
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Li J, Zhou Y, Qin Y, Wei J, Shigong P, Ma H, Li Y, Yuan X, Zhao L, Yan H, Zhang Y, Yu Z. Assessment of the juvenile vulnerability of symbiont-bearing giant clams to ocean acidification. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 812:152265. [PMID: 34902424 DOI: 10.1016/j.scitotenv.2021.152265] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/25/2021] [Revised: 11/30/2021] [Accepted: 12/04/2021] [Indexed: 06/14/2023]
Abstract
Ocean acidification (OA) severely affects marine bivalves, especially their calcification processes. However, very little is known about the fate of symbiont-bearing giant clams in the acidified oceans, which hinders our ability to develop strategies to protect this ecologically and economically important group in coral reef ecosystems. Here, we explored the integrated juvenile responses of fluted giant clam Tridacna squamosa (Lamarck, 1819) to acidified seawater at different levels of biological organization. Our results revealed that OA did not cause a significant reduction in survival and shell growth performance, indicating that T. squamosa juveniles are tolerated to moderate acidification. Yet, significantly reduced net calcification rate demonstrated the calcifying physiology sensitivity to OA, in line with significant declines in symbiont photosynthetic yield and zooxanthellae density which in turn lowered the amount of energy supply for energetically expensive calcification processes. Subsequent transcriptome sequencing and comparative analysis of differentially expressed genes revealed that the regulation of calcification processes, such as transport of calcification substrates, acid-base regulation, synthesis of organic matrix in the calcifying fluid, as well as metabolic depression were the major response to OA. Taken together, the integration of physiological and molecular responses can provide a comprehensive understanding of how the early life history stages of giant clams respond to OA and make an important leap forward in assessing their fate under future ocean conditions.
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Affiliation(s)
- Jun Li
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Yinyin Zhou
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Yanpin Qin
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Jinkuan Wei
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Pengyang Shigong
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Haitao Ma
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Yunqing Li
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Xiangcheng Yuan
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China
| | - Liqiang Zhao
- College of Fisheries, Guangdong Ocean University, Zhanjiang 524088, China
| | - Hong Yan
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
| | - Yuehuan Zhang
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China.
| | - Ziniu Yu
- Key Laboratory of Tropical Marine Bio-resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, Innovation Academy of South China Sea Ecology and Environmental Engineering, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 510301, China; Hainan Key Laboratory of Tropical Marine Biotechnology, Hainan Sanya Marine Ecosystem National Observation and Research Station, Sanya Institute of Oceanology Chinese Academy of Sciences, Sanya 572024, China.
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