4.3 Article

Sediment characteristics of tropical, karst lakes and their relationship with watershed topography, lake morphometry, and human activities

Journal

JOURNAL OF PALEOLIMNOLOGY
Volume 66, Issue 3, Pages 333-353

Publisher

SPRINGER
DOI: 10.1007/s10933-021-00210-z

Keywords

Sediment grain size; Sediment texture; Sediment elemental composition; Eutrophication; Lagunas de Montebello; Chiapas; Mexico

Funding

  1. Fondo Sectorial de Investigacion y Desarrollo Sobre el Agua (Sectorial Fund for Water Research and Development) (CONAGUACONACYT) [167603]
  2. Direccion General de Asuntos del Personal Academico (UNAM-DGAPA-PAPIIT) [IN219215, IV200319]
  3. Comite de Administracion de Tziscao

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The study analyzed sediment characteristics from 18 tropical karst lakes in Lagunas de Montebello National Park, Mexico, and found that differences in topography/location and human activities influenced the sediment composition. Lakes in different regions exhibited variations in sediment texture and organic content, with eutrophication being a key factor in modifying sediment characteristics. Urbanization and agriculture have also played a role in altering sediment properties.
We analyzed multiple variables in recent sediments from 18 tropical, karst lakes in Lagunas de Montebello National Park, a Mexican Protected Natural Area and Ramsar site, to explore relationships between sediment characteristics and lake attributes: topography/location (mountain, surface-water-dominated vs. plateau, groundwater-dominated), morphometry (shallow vs. deep), and human activities (urbanization/agriculture). The study lakes fell into two groups: (1) pristine, oligotrophic, mostly located in the SE mountain terrain, and (2) impacted, eutrophic, in the NW plateau region. Sediment samples were collected from the central, deepest zone of each lake and analyzed for texture (grain size), carbonate content, and organic C and N. Water variables were measured in the water column overlying the sediment collection sites. Specific conductance, chlorophyll a, and total particulate carbon were higher in impacted, eutrophic plateau lakes than in pristine mountain lakes. Sediments, although composed mostly of silts, differed in grain size. Pristine, oligotrophic mountain lakes possessed coarser sediments, with a higher concentration of most likely recalcitrant organic carbon, than impacted, eutrophic plateau lakes. Topography/location is the primary factor that contributes to sediment differences, whereas eutrophication, caused by deforestation and agricultural runoff, is the second most important agent modifying sediment characteristics. The only pristine plateau lake, San Jose, had water quality similar to pristine mountain lakes, but finer sediments with lower organic C, N, and C/N. Comparison of San Jose sediments with those of impacted eutrophic plateau lakes indicated eutrophication has led to coarser sediments, as well as enrichment in CO3, organic C and N. Eutrophication-related sediment characteristics are valuable variables that can be used in paleolimnological studies to identify the onset of lake eutrophication in tropical karst water bodies.

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