Ostracode and C/N based paleoecological record from Santiaguillo basin of subtropical Mexico over last 27 cal kyr BP
Changes in ostracode species assemblage suggest presence of oligohaline and mesohaline waters in the Santiaguillo basin of subtropical Mexico over the last ca. 27 cal kyr BP. Paleoecological reconstruction is based on the distribution of Limnocythere bradburyi Forester, Eucandona cf. patzcuaro Tress...
| Autores: | , , , , |
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| Tipo de documento: | artigo |
| Estado: | Versão publicada |
| Data de publicação: | 2015 |
| País: | México |
| Recursos: | Universidad Nacional Autónoma de México |
| Repositório: | Redalyc-UNAM |
| OAI Identifier: | oai:redalyc.org:57237105001 |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=57237105001 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Ciencias de la Tierra Mexico N ratio Paleoecology Late Quaternary Santiaguillo basin |
| Resumo: | Changes in ostracode species assemblage suggest presence of oligohaline and mesohaline waters in the Santiaguillo basin of subtropical Mexico over the last ca. 27 cal kyr BP. Paleoecological reconstruction is based on the distribution of Limnocythere bradburyi Forester, Eucandona cf. patzcuaro Tressler, Cypridopsis vidua Brady and Limnocythere ceriotuberosa Delorme. Source of organic productivity is inferred from C/N ratios. The basin hosted shallow and oligohaline water during the late glacial (ca.27–19 cal kyr BP) and lacustrine phytoplankton contributed to the organic productivity. However, the water body of Last Glacial Maximum (LGM) was relatively warmer (>13°C) and more diluted compared to the pre-LGM. Increased salinity and reduced lacustrine productivity at ca.19 cal kyr BP marked a shift in the paleoecological conditions. Water body was mesohaline during ca.9.5–4 cal kyr BP and periodic desiccation of the basin possibly caused the absence of ostracode valves in sediments of the last ca.3.5 cal kyr BP. Comparison with other proxy-records from the region indicates that the hydrological variations in different parts of subtropical north and northwestern Mexico were not synchronous during the late Pleistocene and Holocene. |
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