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Citation: Conci, Nicola and Griesshaber, Erika and Rivera, Ramon and Schmahl, Wolfgang and Vargas, Sergio and Wörheide, Gert: Molecular and mineral responses of corals grown under artificial Calcite Sea conditions. 14. March 2023. Open Data LMU. 10.5282/ubm/data.373

Molecular and mineral responses of corals grown under artificial Calcite Sea conditions
Molecular and mineral responses of corals grown under artificial Calcite Sea conditions

The formation of skeletal structures composed of different calcium carbonate polymorphs (aragonite and calcite) appears to be regulated both biologically and environmentally. Among environmental factors influencing aragonite and calcite precipitation, changes in seawater conditions – primarily in the molar ratio of magnesium and calcium during so-called “Calcite” (mMg:mCa below 2) or “Aragonite” seas (mMg:mCa above 2) – have had profound impacts on the distribution and performance of marine calcifiers throughout the Earth’s history. Nonetheless, the fossil record shows that some species appear to have counteracted such changes and kept their skeleton polymorph unaltered. Here, the aragonitic octocoral Heliopora coerulea and the aragonitic scleractinian Montipora digitata were exposed to Calcite Sea-like mMg:mCa with various levels of changes in magnesium and calcium concentration, and both mineralogical (i.e., CaCO3 polymorph) and gene expression changes were monitored. Both species maintained aragonite deposition at lower mMg:mCa ratios, while concurrent calcite presence was only detected in M. digitata. Despite a strong variability between independent experimental replicates for both species, the expression for a set of putative calcification-related genes, including known components of scleractinian skeleton organic matrix, was found to consistently change at lower mMg:mCa. These results support previously proposed involvements of the skeleton organic matrix in counteracting decreases in seawater mMg:mCa. Although no consistent changes in expression for calcium and magnesium transporters was observed, down-regulation calcium channels in H. coerulea in one experimental replicate and at a mMg:mCa of 2.5 might indicate the possibility of active calcium uptake regulation by the corals under altered mMg:mCa open.

Biomineralization, Corals, Calcite seas, Skeleton organic matrix
Conci, Nicola
Griesshaber, Erika
Rivera, Ramon
Schmahl, Wolfgang
Vargas, Sergio
Wörheide, Gert
2023

[thumbnail of SEM Files for: Heliopora coerulea Calcite Sea Experiment] Other (SEM Files for: Heliopora coerulea Calcite Sea Experiment)
Heliopora_coerulea_CalciteSea_Experiments_SEM_files.tar.gz - Other

570MB

DOI: 10.5282/ubm/data.373

This dataset is available unter the terms of the following Creative Commons LicenseCC BY 4.0

Abstract

The formation of skeletal structures composed of different calcium carbonate polymorphs (aragonite and calcite) appears to be regulated both biologically and environmentally. Among environmental factors influencing aragonite and calcite precipitation, changes in seawater conditions – primarily in the molar ratio of magnesium and calcium during so-called “Calcite” (mMg:mCa below 2) or “Aragonite” seas (mMg:mCa above 2) – have had profound impacts on the distribution and performance of marine calcifiers throughout the Earth’s history. Nonetheless, the fossil record shows that some species appear to have counteracted such changes and kept their skeleton polymorph unaltered. Here, the aragonitic octocoral Heliopora coerulea and the aragonitic scleractinian Montipora digitata were exposed to Calcite Sea-like mMg:mCa with various levels of changes in magnesium and calcium concentration, and both mineralogical (i.e., CaCO3 polymorph) and gene expression changes were monitored. Both species maintained aragonite deposition at lower mMg:mCa ratios, while concurrent calcite presence was only detected in M. digitata. Despite a strong variability between independent experimental replicates for both species, the expression for a set of putative calcification-related genes, including known components of scleractinian skeleton organic matrix, was found to consistently change at lower mMg:mCa. These results support previously proposed involvements of the skeleton organic matrix in counteracting decreases in seawater mMg:mCa. Although no consistent changes in expression for calcium and magnesium transporters was observed, down-regulation calcium channels in H. coerulea in one experimental replicate and at a mMg:mCa of 2.5 might indicate the possibility of active calcium uptake regulation by the corals under altered mMg:mCa open.

Uncontrolled Keywords

Biomineralization, Corals, Calcite seas, Skeleton organic matrix

Item Type:Data
Contact Person:Wörheide, Gert
E-Mail of Contact:woerheide at lmu.de
Subjects:Geosciences
Dewey Decimal Classification:500 Natural sciences and mathematics
500 Natural sciences and mathematics > 550 Earth sciences
500 Natural sciences and mathematics > 560 Paleontology, Paleozoology
500 Natural sciences and mathematics > 570 Life sciences
500 Natural sciences and mathematics > 590 Zoological sciences
ID Code:373
Deposited By: Dr Sergio Vargas
Deposited On:22. Mar 2023 08:47
Last Modified:22. Mar 2023 08:47

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