Ostracods are small bivalved aquatic crustancean. They secrete shells of low-Mg calcite that are often preserved in lake sediments. Recent work has shown that the uptake of trace elements (especially Mg and Sr) into the shell may be a function of the salinity and temperature of the host water. Furthermore, ostracod shells are a source of carbonate for stable-isotope analysis. This paper reviews the application of ostracod shell chemistry to Quaternary palaeolimnology. Although such work has revealed the excellent potential of these techniques to provide quantitative palaeolimnological reconstructions, a number of problems have also emerged. These problems relate to (1) methods used for extraction of ostracod shells from sediment and their subsequent cleaning (2) post-mortem diagenesis and alteration of the shell (3) complications with the calcification mechanism (4) spatial and temporal variability in shell composition (5) the ecological tolerances of individual species and (6) the relationships between shell chemistry and palaeohydrology. To some extent, these problems are an inevitable outcome of the diversity of lacustrine systems: they may be overcome by developing a thorough understanding of the physiology, life-cycle and ecology of the species concerned, together with the modern limnology of the study site. Overall, these techniques have excellent potential in Quaternary palaeolimnology, especially when used with other palaeoenvironmental indicators.
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Anadón, P. & R. Juliá, 1990. Hydrochemistry from Sr and Mg content of ostracodes in Pleistocene lacustrine deposits, Baza Basin (SE Spain). Hydrobiologia 197: 291–303.
Anadón, P., R. Juliá & R. Utrilla, 1994. Palaeoenvironmental reconstruction from faunal assemblages and ostracode shell geochemistry of a Pleistocene lacustrine sequence, Baza Basin, SE Spain. Palaeogeogr. Palaeoclim. Palaeoecol. 111: 191–205.
Benson, L. V., P. A. Meyers & R. J. Spencer, 1991. Change in the size of Walker Lake during the past 5000 years. Palaeogeogr. Palaeoclim. Palaeoecol. 81: 189–214.
Boomer, I., 1993. Palaeoenvironmental indicators from Late Holocene and contemporary Ostracoda of the Aral Sea. Palaeogeogr. Palaeoclim. Palaeoecol. 103: 141–153.
Boyle, E. A., 1981. Cadmium, zinc, copper and barium in Foraminifera tests. Earth planet. Sci. Lett. 53: 111–135.
Bridgwater, N. D., 1995. Non-marine ostracods as indicators of Holocene environmental change in Central Mexico. Unpubl. PhD Thesis, Kingston University, UK, 298 pp.
Cadot, H. M., R. L. Kaesler & W. R. V. Schmus, 1975. Application of the electron microprobe analyzer to the study of the ostracode carapace. In, F. M. Swain, (ed) Biology and paleobiology of Ostracoda. Bull. am. Palaeont. 65: 577–585.
Cadot, H. M., W. R. V. Schmus & R. L. Kaesler, 1972. Magnesium in calcite of marine Ostracoda. Bull. geol. Soc. Am. 83: 3519–3522.
Chivas, A. R., P.De Deckker & J. M. G. Shelley, 1983. Magnesium, strontium and barium partitioning in nonmarine ostracode shells and their use in paleoenvironmental reconstructions — a preliminary study. In, R. F. Maddocks, (ed) Applications of Ostracoda. The University of Houston, Houston: 238–249.
Chivas, A. R., P.De Deckker & J. M. G. Shelley, 1985. Strontium content of ostracods indicates lacustrine palaeosalinity. Nature 316: 251–253.
Chivas, A. R., P.De Deckker & J. M. G. Shelley, 1986a. Magnesium and strontium in non-marine ostracod shells as indicators of palaeosalinity and palaeotemperature. Hydrobiologia 143: 135–142.
Chivas, A. R., P.De Deckker & J. M. G. Shelley, 1986b. Magnesium content of non-marine ostracod shells: a new palaeosalinometer and palaeothermometer. Palaeogeogr. Palaeoclim. Palaeoecol. 54: 43–61.
Chivas, A. R., P. De Deckker, J. A. Cali, A. Chapman, E. Kiss & J. M. G. Shelley, 1993. Coupled stable isotope and trace-element measurements of lacustrine carbonates as paleoclimatic indicators. In, P. K. Swart, K. C. Lohmann, J. McKenzie & S. Savin, (eds) Climate change in continental isotopic records. Am. geophys. Union geophys. Monogr. 78: 113–121.
Colman, S. M., L. D. Keigwin & R. M. Forester, 1994. Two episodes of meltwater influx from glacial Lake Agassiz into the Lake Michigan basin and their climatic contrasts. Geology 22: 547–550.
Curtis, J. H. & D. A. Hodell, 1993. An isotopic and trace element study of ostracods from Lake Mirggoane, Haiti: A 10 500 year record of paleosalinity and paleotemperature changes in the Caribbean. In, P. K. Swart, K. C. Lohmann, J. McKenzie & S. Savin, (eds) Climate change in continental isotopic records. Am. geophys. Union geophys. Monogr. 78: 113–121.
Delorme, L. D., 1969. Ostracodes as Quaternary palaeo-ecological indicators. Can. J. Earth Sci. 6: 1471–1476.
Delorme, L. D., 1978. Distribution of freshwater ostracodes in Lake Erie. J. Great Lakes Res. 4: 216–220.
Dettman, D. L., A. J. Smith, D. K. Rea, T. C. Moore & K. C. Lohmann, 1995. Glacial meltwater in Lake Huron inferred from single-valve analysis of oxygen isotopes in ostracodes. Quat. Res. 43: 297–310.
Durazzi, J. T., 1975. The shell chemistry of ostracods and its paleoecological significance. Unpubl. PhD Thesis, Case Western Reserve University, Cleveland, Ohio, USA, 192 pp.
Durazzi, J. T., 1977. Stable isotopes in the ostracod shell: a preliminary study. Geochim. Cosmochim. Acta 41: 1168–1170.
Engstrom, D. R. & S. R. Nelson, 1991. Paleosalinity from trace metals in fossil ostracodes compared with observational records at Devils Lake, North Dakota, USA. Palaeogeogr. Palaeoclim. Palaeoecol. 83: 295–312.
Engstrom, D. R., J. Xia & E. Ito, 1993. A study of the variability of Mg/Ca and Sr/Ca in ostracode calcite by laboratory culture and field collection. EOS Trans. am. geophys. Union 74: 365.
Eyles, N. & H. P. Schwarz, 1991. Stable isotope record of the last glacial cycle from lacustrine ostracodes. Geology 19: 257–260.
Forester, R. M., 1983. Relationship of two lacustrine ostracode species to solute composition and salinity: implications for paleohydrochemistry. Geology 11: 435–438.
Forester, R. M., 1986. Determination of the dissolved anion composition of ancient lakes from fossil ostracodes. Geology 14: 796–798.
Forester, R. M., S. M. Colman, R. L. Reynolds & L. D. Keigwin, 1994. Lake Michigan's late Quaternary limnological and climate history from ostracode, oxygen isotope and magnetic susceptibility. J. Great Lakes Res. 20: 93–107.
Francus, P., S. Leroy, I. Mergeai, G. Seret & G. Wansard, 1993. A Multidisciplinary study of the Vico Maar sequence (Latium, Italy): part of the last cycle in the Mediterranean area. Preliminary results. In, J. F. W. Negendank & B. Zolitschka, (eds) Paleolimnology of European maar lakes. Lecture Notes in Earth Sciences. Berlin, Springer-Verlag 49: 289–304.
Fritz, S. C., D. R. Engstrom & B. J. Haskell, 1994. ‘Little Ice Age’ aridity in the North American Great Plains: a high-resolution reconstruction of salinity fluctuations from Devils Lake, North Dakota, USA. The Holocene 4: 69–73.
Fritz, P., T. W. Anderson & C. F. M. Lewis, 1975. Late Quaternary climatic trends and history of Lake Erie from stable isotope studies. Science 190: 267–269.
Gasse, F., J. C. Fontes, J. C. Plaziat, P. Carbonel, I. Maczmarska, P.De Deckker, I. Soulie-Marsche, Y. Callot & P. A. Dupeuple, 1987. Biological remains, geochemistry and stable isotopes for the reconstruction of environmental and hydrological changes in the Holocene lakes from North Sahara. Palaeogeogr. Palaeoclim. Palaeoecol. 60: 1–46.
Hammarlund, D. & G. Lemdahl, 1994. A Late Weichselian stable isotope stratigraphy compared with biostratigraphical data: a case study from southern Sweden. J. Quat. Sci. 9: 13–31.
Hammarlund, D. & D. H. Keen, 1994. A Late Weichselian stable isotope and molluscan stratigraphy from southern Sweden. Geol. För. Stock. Förh. 116: 235–248.
Hardie, L. A. & H. P. Eugster, 1970. The evolution of closed-basin brines. Min. Soc. Am. Spec. Paper 3: 273–290.
Heaton, T. H. E., J. A. Holmes & N. D. Bridgwater, in press. Carbon and oxygen isotope variations among lacustrine ostracods: implications for palaeoclimatic studies. The Holocene.
Henderson, P. A., 1990. Freshwater Ostracods. Synopses of the British Fauna (New Series), No. 42. UBS/Dr W. Backhuys, Oegstgeest, 228 pp.
Hodell, D. A., J. H. Curtis, G. A. Jones, A. Higuera-Grundy, M. Brenner, M. W. Binford & K. T. Dorsey, 1991. Reconstruction of Caribbean climate change over the past 10 500 years. Nature 352: 790–793.
Hodell, D. A., J. H. Curtis & M. Brenner, 1995. Possible role of climate in the collapse of Classic Maya civilization. Nature 375: 391–394.
Hodgkinson, R. L., 1991. Microfossil processing: a damage report. Micropaleontology 37: 320–326.
Holmes, J. A., 1992a. Nonmarine ostracods as Quaternary palaeoenvironmental indicators. Prog. Phys. Geog. 16: 405–431.
Holmes, J. A., 1992b. Micropalaeontology notebook. Trace-element chemistry of non-marine ostracod shells: a preliminary evaluation of cleaning methods. J. Micropalaeont. 11: 36.
Holmes, J. A., P. E. Hales & F. A. Street-Perrott, 1992. Trace-element chemistry of non-marine ostracods as a means of palaeolimnological reconstruction. An example from the Quaternary of Kashmir, northern India. Chem. Geol. 95: 177–186.
Holmes, J. A., F. A. Street-Perrott, M. Ivanovich & R. A. Perott, 1995a. A late Quaternary palaeolimnological record from Jamaica based on trace-element chemistry of ostracod shells. Chem. Geol. 124: 143–160.
Holmes, J. A., F. A. Street-Perrott, T. H. E. Heaton, D. P. F. Darbyshire, N. C. Davies & P. E. Hales. 1995b. Chemical and isotopic composition of karstic lakes in Jamaica, West Indies. Hydrobiologia 312: 121–138.
Kelts, K. & M. R. Talbot, 1990. Lacustrine carbonates as geochemical archives of environmental change and biotic/abiotic interactions. In, M. M. Tilzer & C. Serruya (eds), Large Lakes: Ecological Structure and Function. Science and Technology Publishers, Madison, 288–315.
Kesling, R. V., 1951. Terminology of ostracod carapaces. Contrib. Mus. Paleontol. Univ. Michigan 9: 93–171.
Lamb, H. F., F. Gasse, A. Benkaddour, N.El Hamouti, S.van der Kaars, W. T. Perkins, N. J. Pearce & C. N. Roberts, 1995. Relation between century-scale Holocene arid intervals in tropical and temperate zones. Nature 373: 134–137.
Last, W. M., J. T. Teller & R. M. Forester, 1994. Paleohydrology and paleochemistry of Lake Manitoba, Canada: the isotope and ostracode records. J. Paleolimnol. 12: 269–282.
Lewis, C. F. M. & T. W. Anderson, 1992. Stable isotope (O and C) and pollen trends in eastern Lake Erie, evidence for a locally-induced climatic reversal of Younger Dryas age in the Great Lakes Basin. Clim. Dyn. 6: 241–250.
Lister, G. S., 1988. A 15 000 year isotopic record from Lake Zürich of deglaciation and climatic change in Switzerland. Quart. Res. 29, 129–141.
Lister, G. S., 1989. Reconstruction of palaeo air temperature changes from oxygen isotopic records in Lake Zürich: the significance of seasonality. Eclogae geol. Helv. 82: 219–234.
Lister, G. S., K. Kelts, K. Z. Chen, Y. Jun-Qing & F. Niessen, 1991. Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for Ostracoda since the latest Pleistocene. Palaeogeogr. Palaeoclim. Palaeoecol. 84: 141–162.
McCulloch, M. T. & P.De Deckker, 1989. Sr isotope constraints on the Mediterranean environment at the end of the Messinian Salinity crisis. Nature 342: 62–65.
McKenzie, J. A., 1985. Carbon isotopes and productivity in the lacustrine and marine environment. In W. Stumm (ed), Chemical processes in lakes. Wiley, New York: 99–118.
Mourguiart, P., P. Carbonel, J.-P. Peypouquet, D. Wirrmann, & C. Vargas, 1986. Late Quaternary palaeohydrology of Lake Huinaymarca (Bolivia). Hydrobiologia 143: 191–197.
Neale, J. W., 1988. Ostracods and palaeosalinity reconstruction. In, P.De Deckker, J.-P. Colin & J.-P. Peypouquet, (eds) Ostracoda in the Earth Sciences, Amsterdam, Elsevier 125–155.
Niessen, F. & K. Kelts, 1989. The deglaciation and Holocene sedimentary evolution of southern perialpine Lake Lugano—implications for Alpine paleoclimate. Ecologia geol. Helv. 82: 235–263.
Palacios-Fest, M. R., 1994. Nonmarine ostracode shell chemistry from ancient Hohokam irrigation canals in central Arizona: a paleohydrological tool for the interpretation of prehistoric human occupation in the North American southwest. Geoarchacology 9: 1–29.
Palacios-Fest, M. R. & A. S. Cohen, 1993. Non-marine ostracode shell chemistry as a paleohydrochemical indicator: assumptions and constraints In, K. G. McKenzie & P. J. Jones, (eds) Ostracoda in the Earth and Life Sciences. Proceedings of the 11th International Symposium on Ostracoda, Warrnambool, Australia, A.A. Balkema, Rotterdam: 680–681.
Palacios-Fest, M. R., A. S. Cohen & P. Anadón, 1994. Use of ostracodes as paleoenvironmental tools in the interpretation of ancient lacustrine records. Rev. esp. Paleontol. 9: 145–164.
Palacios-Fest, M. R., A. S. Cohen, J. Ruiz & B. Blank, 1993. Comparative paleoclimatic interpretations from nonmarine ostracodes using faunal assemblages, trace elements shell chemistry and stable isotope data. In, P. K. Swart, K. C. Lohmann, J. McKenzie & S. Savin, (eds) Climate change in continental isotopic records. Am. geophys. Union geophys. Monogr. 78: 179–190.
Rea, D. K., T. C. Moore, C. F. M. Lewis, L. A. Meyer, D. L. Dettman, A. J. Smith & D. M. Dobson, 1994. Stratigraphy and paleolimnologic record of lower Holocene sediments in northern Lake Huron and Georgian Bay. Can. J. Earth Sci. 31: 1586–1605.
Rogers, K. L., 1993. A comparison of stable isotope data with pollen and ostracod faunal data in paleoclimate reconstruction In, P. K. Swart, K. C. Lohmann, J. McKenzie & S. Savin, (eds) Climate change in continental isotopic records. Am. geophys. Union geophys. Monogr. 78: 203–215.
Rogers, K. L., E. E. Larson, G. Smith, D. Katzman, G. R. Smith, T. Cerling, Y. Wang, R. G. Baker, K. C. Lohman, C. A. Repenning, P. Patterson & G. Mackie 1992. Pliocene and Pleistocene geologic and climatic evolution in the San Luis Valley of south-central Colorado. Palaeogeogr. Palaeoclim. Palaeoecol. 94: 55–86.
Schwalb, A., G. S. Lister & K. Kelts, 1994. Ostracode carbonate δ18O and δ13C signatures of hydrological and climatic changes affecting lake Neuchâtel, Switzerland, since the latest Pleistocene. J. Paleolimnol. 11: 3–17.
Schwalb, A., S. M. Locke & W. E. Dean, 1994. Ostracode δ18O and δ13C evidence of Holocene environmental changes in the sediments of two Minnesota lakes. J. Paleolimnol. 14: 281–296.
Slipper, I. J., 1992. Early Turonian Ostracoda: The Melbourn Rock fauna from Abbots Cliff, Dover, England. 2nd European Ostracodologists' Meeting, Glasgow, UK. Preprints of papers: 199–208.
Sohn, I. G., 1958. Chemical constituents of ostracodes: some applications to paleontology and paleoecology. J. Paleont. 32: 730–736.
Street-Perrott, F. A., P. E. Hales, R. A. Perrott, J. Ch. Fontes, V. R. Switsur & A. Pearson, 1993. Limnology and palaeolimnology of a tropical marl lake: Wallywash Great Pond, Jamaica. J. Paleolimnol. 9: 322.
Stuiver, M., 1970. Oxygen and carbon isotope ratios as climatic indicators. J. geophys. Res. 75: 5247–5257.
Talbot, M. R., 1990. A review of the palaeohydrological interpretation of carbon and oxygen isotopes in primary lacustrine carbonates. Chem. Geol. (Isot. Geosci. Sect.) 80: 261–279.
Tardy, Y., C. Cheverry & B. Fritz, 1974. Néoformation d'une argile magnésienne dans les dépressions interdunaires du lac Tchad. Application aux domaines de stabilité des phyllosilicates alumineux, magnésiens et ferrifères. C. R. acad. Sc. Paris. 278: 1999–2002.
Teeter, J. W. & T. J. Quick, 1990. Magnesium-salinity relation in the saline lake ostracode Cyprideis Americana. Geology 18: 220–222.
Turpen, J. B. & R. W. Angell, 1971. Aspects of molting and calcification in the ostracode Heterocypris. Biol. Bull. 140: 331–338.
Von Grafenstein, U., H. Erlenkeuser, J. Müller & A. Kleinmann-Eisenmann, 1992. Oxygen isotope records of benthic ostracods in Bavarian lake sediments. Naturwissenschaften 79: 145–152.
Von Grafenstein, U., H. Erlenkeuser, A. Kleinmann, J. Müller & P. Trimborn, 1994. High-frequency climatic oscillations during the last deglaciation as revealed by oxygen-isotope records of benthic organisms (Ammersee, southern Germany). J. Paleolimnol. 11: 349–357.
Whitmore, T. J., M. Brenner, J. H. Curtis, B. H. Dahlin & B. Leyden, in press. Holocene climatic and human influences on lakes of Yucatan Peninsula, Mexico. The Holocene.
Xia, J., E. Ito & D. R. Engstrom, 1993. Oxygen isotope composition of lacustrine ostracodes as paleoclimate indicator. EOS Trans. am. geophys. Union 74: 365.
Xia, J., E. Ito & D. R. Engstrom, 1994. A study of combined stable-isotope and trace-element composition in lacustrine ostracodes as paleoclimatic indicators in the northern Great Plains, North American Abstracts, 8th International Conference on Geochronology, Cosmochronology & Isotope Geology, Berkeley, 356.
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Holmes, J.A. Trace-element and stable-isotope geochemistry of non-marine ostracod shells in Quaternary palaeoenvironmental reconstruction. J Paleolimnol 15, 223–235 (1996). https://doi.org/10.1007/BF00213042
- trace elements
- stable isotopes