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Paleoenvironmental implications of carbon stable isotope composition of land snail tissues

Published online by Cambridge University Press:  20 January 2017

Yurena Yanes ,
María P. Asta ,
Miguel Ibáñez ,
María R. Alonso  and
Christopher S. Romanek
Yurena Yanes*
Affiliation:
Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA Instituto Andaluz de Ciencias de la Tierra (CSIC-Universidad de Granada), Avenida Las Palmeras 4, 18100 Armilla, Granada, Spain
María P. Asta
Affiliation:
Instituto Andaluz de Ciencias de la Tierra (CSIC-Universidad de Granada), Avenida Las Palmeras 4, 18100 Armilla, Granada, Spain
Miguel Ibáñez
Affiliation:
Departamento de Biologia Animal, Universidad de La Laguna, E-38206 La Laguna, Tenerife, Islas Canarias, Spain
María R. Alonso
Affiliation:
Departamento de Biologia Animal, Universidad de La Laguna, E-38206 La Laguna, Tenerife, Islas Canarias, Spain
Christopher S. Romanek
Affiliation:
Department of Earth and Environmental Sciences, University of Kentucky, Lexington, KY 40506, USA
*
*Corresponding author at: Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA. E-mail address:[email protected] (Y. Yanes).
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Abstract

Land snail shell δ13C value is often used as a paleovegetation proxy assuming that snails ingest all plants in relation to their abundance, and that plants are the only source of carbon. However, carbonate ingestion and variable metabolic rates complicate these relationships. We evaluate if live-collected snails from Lanzarote (Canary Islands) reflect the abundance of C3 and CAM plants. Snails were collected on either CAM or C3 plants for isotope analysis of shell and body, and shell size. Respective shell and body δ13C values of snails collected on CAM plants averaged − 8.5 ± 1.7‰ and − 22.8 ± 1.6‰, whereas specimens from C3 plants averaged − 10.1 ± 0.7‰ and − 24.9 ± 1.1‰. A flux balance model suggests snails experienced comparable metabolic rates. A two-source mass balance equation implies that snails consumed ~ 10% of CAM, which agrees with their abundance in the landscape. Snails collected on CAM plant were smaller than those on C3 plants. Conclusively: 1) snails consume CAM plants when they are available; 2) migration of snails among C3 and CAM plants is a common phenomenon; and 3) C3 plants may be a more energetic food for growth than CAM plants. This study shows that shell δ13C values offer approximate estimates of plants in C3–CAM mixed environments.

Keywords

Land snailsStable isotopesC3 and CAM plantsPaleoenvironmentLanzaroteCanary Islands
Type
Original Articles
Information
Quaternary Research , Volume 80 , Issue 3 , November 2013 , pp. 596 - 605
Copyright
University of Washington

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References

Balakrishnan, M., Yapp, C.J., (2004). Flux balance model for the oxygen and carbon isotope compositions of land snail shells. Geochimica et Cosmochimica Acta 68, 2007–2024.Google Scholar
Balakrishnan, M., Yapp, C.J., Theler, J.L., Carter, B.J., Wyckoff, D.G., (2005). Environmental significance of 13C/12C and 18O/16O ratios of modern land-snail shells from the southern Great Plains of North America. Quaternary Research 63, 15–30.Google Scholar
Baldini, L.M., Walker, S.E., Bruce, R., Baldini, J.U.L., Crowe, D.E., (2007). Isotope ecology of the modern land snails Cerion, San Salvador, Bahamas: preliminary advances toward establishing a low-latitude island palaeoenvironmental proxy. Palaios 22, 174–187.Google Scholar
Chiba, S., Davison, A., (2009). Associations between the shell stable carbon isotope and vegetation in modern and fossil land snails Mandarina cichijimana on Chichijima of the Ogasawara Islands. Paleontological Research 13, 151–157.Google Scholar
Clementz, M.T., (2012). New insight from old bones: stable isotope analysis of fossil mammals. Journal of Mammalogy 93, 368–380.Google Scholar
Dawson, T.E., Mambelli, S., Plamboeck, A.H., Templer, PlH, Tu, K.P., (2002). Stable isotopes in plant ecology. Annual Review of Ecology and Systematics 33, 507–559.Google Scholar
DeNiro, M.J., Epstein, S., (1978). Influence of diet on the distribution of carbon isotopes in animals. Geochimica et Cosmochimica Acta 42, 495–506.CrossRefGoogle Scholar
Farquhar, G.D., Ehleringer, J.R., Hubick, K.T., (1989). Carbon isotope discrimination and photosynthesis. Annual Review of Plant Physiology and Plant Molecular Biology 40, 503–537.Google Scholar
Fernández-Palacios, J.M., Whittaker, R.J., (2008). The Canaries: an important biogeographical meeting place. Journal of Biogeography 35, 379–387.Google Scholar
Goodfriend, G.A., (1986). Variation in land snail shell form and size and its causes: a review. Systematic Zoology 35, 204–223.Google Scholar
Goodfriend, G.A., (1987). Radiocarbon age anomalies in shell carbonate of land snails from semi-arid areas. Radiocarbon 29, 159–167.Google Scholar
Goodfriend, G.A., (1990). Rainfall in the Negev Desert during the Middle Holocene, Based on 13C of Organic Matter in Land Snail Shells. Quaternary Research 34, 186–197.Google Scholar
Goodfriend, G.A., Ellis, G.L., (2000). Stable carbon isotope record of middle to late Holocene climate changes from land snail shells at Hinds Cave. Texas. Quaternary International 67, 47–60.Google Scholar
Goodfriend, G.A., Ellis, G.L., (2002). Stable carbon and oxygen isotope variations in modern Rabdotus land snail shells in the southern Great Plains, USA, and their relation to environment. Geochimica et Cosmochimica Acta 66, 1987–2002.Google Scholar
Goodfriend, G.A., Hood, D.G., (1983). Carbon isotope analysis of land snail shells: implications for carbon sources and radiocarbon dating. Radiocarbon 25, 810–830.Google Scholar
Goodfriend, G.A., Ellis, G.L., Toolin, L.J., (1999). Radiocarbon age anomalies in land snail shells from Texas: ontogenetic, individual and geographic patterns of variation. Radiocarbon 41, 149–156.CrossRefGoogle Scholar
Hammer, O., Harper, D.A.T., Ryan, P.D., (2001). PAST: paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4, 1.Google Scholar
Hausdorf, B., (2006). Is the interspecific variation of body size of land snails correlated with rainfall in Israel and Palestine?. Acta Oecologica 30, 374–379.Google Scholar
Huntley, J.W., Yanes, Y., Kowalewski, M., Castillo, C., Delgado-Huertas, A., Ibáñez, M., Alonso, M.R., Ortiz, J.E., Torres, T., (2008). Testing limiting similarity in Quaternary terrestrial gastropods. Paleobiology 34, 378–388.CrossRefGoogle Scholar
Jahren, A.H., (2004). The carbon stable isotope composition of pollen. Review of Palaeobotany and Palynology 132, 291–313.Google Scholar
Kerney, M.P., Cameron, R.A.D., (1979). A Field Guide to the Land Snails of Britain and North-West Europe. Collins, London.Google Scholar
Koch, P.L., Diffenbaugh, N.S., Hoppe, K.A., (2004). The effects of late Quaternary climate and pCO 2 change on C 4 plant abundance in the south-central United States. Palaeogeography Palaeoclimatology Palaeoecology 207, 331–357.Google Scholar
Metref, S., Rousseau, D.D., Bentaleb, I., Labonne, M., Vianey-Liaud, M., (2003). Study of the diet effect on δ13C of shell carbonate of the land snail Helix aspersa in experimental conditions. Earth and Planetary Science Letters 211, 381–393.Google Scholar
Nelson, D.M., Sheng Hu, F., Michener, R.H., (2006). Stable-carbon isotope composition of Poaceae pollen: an assessment for reconstructing C 3 and C 4 grass abundance. The Holocene 16, 819–825.Google Scholar
O'Leary, M.H., ('Leary, 1981). Carbon isotope fractionation in plants. Phytochemistry 20, 553–567.Google Scholar
Parnell, A., Inger, R., Bearhop, S., Jackson, A.L., (2010). Source partitioning using stable isotopes: coping with too much variation. PloS One 5, e9672 10.1371/journal.pone.0009672.Google Scholar
Perry, R., Arthur, W., (1991). Shell size and population density in large helicid land snails. The Journal of Animal Ecology 60, 409–421.Google Scholar
Phillips, D.L., (2012). Converting isotope values to diet composition: the use of mixing models. Journal of Mammalogy 93, 342–352.CrossRefGoogle Scholar
Quade, J., Cerling, T.E., (1995). Expansion of C 4 grasses in the Late Miocene of Northern Pakistan: evidence from stable isotopes in paleosols. Palaeogeography Palaeoclimatology Palaeoecology 115, 91–116.Google Scholar
Sarakinos, H.C., Johnson, M.L., Vander Zanden, M.J., (2002). A synthesis of tissue-preservation effects on carbon and nitrogen stable isotope signatures. Canadian Journal of Zoology 80, 381–387.CrossRefGoogle Scholar
Speiser, B., (2001). Food and feeding behavior. Barker, G.M. The Biology of Terrestrial Mollusk. CABI, 259–288.Google Scholar
Stott, L.D., (2002). The influence of diet on the δ13C of shell carbon in the pulmonate snail Helix aspersa . Earth and Planetary Science Letters 195, 249–259.Google Scholar
Yanes, Y., Delgado, A., Castillo, C., Alonso, M.R., Ibáñez, M., De la Nuez, J., Kowalewski, M., (2008). Stable isotope (δ18O, δ13C, and δD) signatures of recent terrestrial communities from a low-latitude, oceanic setting: endemic land snails, plants, rain, and carbonate sediments from the eastern Canary Islands. Chemical Geology 249, 377–392.Google Scholar
Yanes, Y., Romanek, C.S., Delgado, A., Brant, H.A., Noakes, J.E., Alonso, M.R., Ibáñez, M., (2009). Oxygen and carbon stable isotopes of modern land snail shells as environmental indicators from a low-latitude oceanic island. Geochimica et Cosmochimica Acta 73, 4077–4099.Google Scholar
Yanes, Y., Yapp, C.J., Ibáñez, M., Alonso, M.R., De la Nuez, J., Quesada, M.L., Castillo, C., Delgado, A., (2011). Pleistocene–Holocene environmental change in the Canary Archipelago as inferred from stable isotopes of land snail shells. Quaternary Research 65, 658–669.Google Scholar
Yanes, Y., García-Alix, A., Asta, M.P., Ibáñez, M., Alonso, M.R., Delgado, A., (2013). Late Pleistocene–Holocene environmental conditions in Lanzarote (Canary Islands) inferred from calcitic and aragonitic land snail shells and bird bones. Palaeogeography Palaeoclimatology Palaeoecology 378, 91–102.Google Scholar
ZongXiu, L., ZhaoYan, G., NaiQin, W., Bing, X., (2007). Diet control on carbon isotopic composition of land snail shell carbonate. Chinese Science Bulletin 52, 388–394.Google Scholar