Schwalb, Antje; Burns, Stephen J; Cusminsky, Gabriela; Kelts, Kerry; Markgraf, Vera (2002): Assemblages and isotopic signals of modern ostracodes and host waters from Patagonia, Argentine [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.663169, Supplement to: Schwalb, A et al. (2002): Assemblage diversity and isotopic signals of modern ostracodes and host waters from Patagonia, Argentina. Palaeogeography, Palaeoclimatology, Palaeoecology, 187(3-4), 323-339, https://doi.org/10.1016/S0031-0182(02)00484-4
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Abstract:
Ostracode species assemblages and stable oxygen and carbon isotope ratios of living and recent ostracodes, together with delta18O and delta13C_DIC values of host water samples, provide a first data set that characterizes a wide range of modern aquatic environments in the Laguna Cari-Laufquen (41°S, 68 - 69°W) and the Lago Cardiel area (48 - 49°S, 70 - 71°W) in Patagonia, Argentina. This data set will ultimately be used to interpret and calibrate data acquired from lake sediment cores with the goal of reconstructing past climate.
Species assemblages and isotope values can be assigned to three groups; (1) springs, seeps and streams, (2) permanent ponds and lakes, and (3) ephemeral ponds and lakes. Springs, seeps and streams are characterized by Darwinula sp., Heterocypris incongruens, Eucypris fontana, Amphicypris nobilis and Ilyocypris ramirezi. Ostracode and water isotope values range between –13 and –5 per mil for oxygen, and between –15 and –3 per mil for carbon. They are the most negative of the entire sample set, reflecting ground water input with little or no evaporative enrichment. Limnocythere patagonica, Eucypris labyrinthica, Limnocythere sp. and Eucypris aff. fontana are typical species of permanent ponds and lakes. Isotope values indicate high degree of evaporation of lake waters relative to feeder springs and streams and range between –7 and +5 per mil for oxygen, and –5 and +4 per mil for carbon. Limnocythere rionegroensis is the dominant species in ephemeral ponds and lakes. These systems display the most enriched isotope values in both ostracodes and host waters, extending from –5 to +7 per mil for oxygen, and from –5 to +6 per mil for carbon. Living ostracodes show a positive offset from equilibrium values of up to 2 per mil for oxygen. Carbon-isotope values are up to 6‰ more negative than equilibrium values in highly productive pools.
Comparison of ostracode and host water isotope signals permits assessment of the life span of the aquatic environments. Valves from dead ostracodes collected from ephemeral ponds and lakes show a wide scatter with each sample providing a snapshot of the seasonal history of the host water. The presence of the stream species Ilyocypris ramirezi and a wide range of ostracode isotope values suggest that ephemeral ponds and lakes are fed by streams during spring run-off and seasonally dry. A temporary character is also indicated by Heterocypris incongruens, a drought-resistant species that occupies most springs and seeps. In addition, Limnocythere rionegroensis has adjusted its reproduction strategies to its environment. Whereas only females were collected in fresh host waters, males were found in ephemeral ponds and lakes with higher solute content. Sexual reproduction seems to be the more successful reproduction strategy in high and variable salinities and seasonal droughts. The temporary character of the aquatic environments shows that the availability of meteoric water controls the life span of host waters and underlines the sensitivity of the area to changes in precipitation.
Coverage:
Median Latitude: -45.271165 * Median Longitude: -69.944552 * South-bound Latitude: -49.000000 * West-bound Longitude: -71.300000 * North-bound Latitude: -41.000000 * East-bound Longitude: -68.000000
Date/Time Start: 1998-01-01T00:00:00 * Date/Time End: 1998-02-28T00:00:00
Event(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
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4 datasets
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Datasets listed in this publication series
- Schwalb, A; Burns, SJ; Cusminsky, G et al. (2002): (Table 4) Major ion composition of host waters for individual ostracode species from Patagonia, Argentina. https://doi.org/10.1594/PANGAEA.663144
- Schwalb, A; Burns, SJ; Cusminsky, G et al. (2002): (Table 3) Stable carbon and oxygen isotope data from bulk sediment and ostracode valves of modern surface sediment samples from Patagonia, Argentina. https://doi.org/10.1594/PANGAEA.663143
- Schwalb, A; Burns, SJ; Cusminsky, G et al. (2002): (Table 2) Ostracode assemblages and environment characteristica of modern surface sediment samples from Patagonia, Argentina. https://doi.org/10.1594/PANGAEA.663142
- Schwalb, A; Burns, SJ; Cusminsky, G et al. (2002): (Table 1) Physical and chemical characteristics of water samples from Patagonia, Argentina. https://doi.org/10.1594/PANGAEA.663132