| one publication added to basket [289240] | Detection of periodic Sr Ca-1 cycles along gastropod statoliths allows the accurate estimation of age
Galante-Oliveira, S.; Marçal, R.; Espadilha, F.; Sá, M.; Abell, R.; Machado, J.; Barroso, C.M. (2015). Detection of periodic Sr Ca-1 cycles along gastropod statoliths allows the accurate estimation of age. Mar. Biol. (Berl.) 162(7): 1473-1483. https://dx.doi.org/10.1007/s00227-015-2684-y
In: Marine Biology: International Journal on Life in Oceans and Coastal Waters. Springer: Heidelberg; Berlin. ISSN 0025-3162; e-ISSN 1432-1793, meer
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| Project | Top | Auteurs |
- Association of European marine biological laboratories, meer
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| Auteurs | | Top |
- Galante-Oliveira, S.
- Marçal, R.
- Espadilha, F.
- Sá, M.
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- Abell, R.
- Machado, J.
- Barroso, C.M.
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| Abstract |
Gastropods retain less obvious periodic growth marks on calcified structures than individuals in other groups (e.g. bivalves, cephalopods, fish), a fact that has hampered age estimation in this Class. Nevertheless, a model of age estimation for the gastropod Nassarius reticulatus is possible based on the annual growth rings deposited in statoliths during the winter. These spherical aragonitic carbonate structures are located inside the statocysts and contain a characteristic microstructural pattern of concentric rings. However, this pattern can be biased by the formation of nonperiodic disturbance rings (DRs). In Aveiro (NW Portugal), an increased frequency of DRs was reported in statoliths of specimens inhabiting the Ria de Aveiro lagoon (a highly dynamic environment), when compared with specimens collected from the relatively environmentally stable adjacent offshore area. One approach to resolve annual growth in organically precipitated carbonates is to find a chemical signature within the microstructure that faithfully records changes in seasonal environmental parameters. In this contribution, we have analysed the Sr Ca−1 variation along statolith sections by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) as a proxy to resolve seasonal cycles of temperature, allowing the identification of annual growth rings. Combining this information with size–frequency distributions of shell height, we found strong evidence that the rings chemically labelled with 88Sr 48Ca−1 peaks are formed annually during the cold season. Hence, LA-ICPMS allows not only the detection of visible rings but also the distinction between rings formed at low temperatures (i.e. a periodic seasonal signature) and those of disturbance (not characterised by increased 88Sr 48Ca−1). There is also clear evidence that the 88Sr 48Ca−1 peaks become less conspicuous from the nucleus to the statolith edge, leading to a loss of discriminatory power for the identification of older age rings. Nevertheless, this new method allows the accurate age estimation of N. reticulatus specimens and is liable to be applied in a wide range of gastropods after specific validation. |
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