2010
DOI: 10.1134/s1064229310130041
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The complex genesis of red soils in peninsula de Yucatán, Mexico: Mineralogical, micromorphological and geochemical proxies

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Cited by 36 publications
(20 citation statements)
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“…Regarding the origin of siderite, that was not present in the limestone rock (Table 3), it is possible that the source of Fe is the redeposited ironclay clusters, observed particularly in thin sections of wetland periphery profiles PY3 and PY4, for example from the Kantunilkin area, as seen in Cabadas et al (2010), which were incorporated in their horizons. Fe then could be reduced in the anoxic wetland soil environment and precipitated as Fe 2+ carbonate.…”
Section: Origin Of Secondary Carbonatesmentioning
confidence: 94%
“…Regarding the origin of siderite, that was not present in the limestone rock (Table 3), it is possible that the source of Fe is the redeposited ironclay clusters, observed particularly in thin sections of wetland periphery profiles PY3 and PY4, for example from the Kantunilkin area, as seen in Cabadas et al (2010), which were incorporated in their horizons. Fe then could be reduced in the anoxic wetland soil environment and precipitated as Fe 2+ carbonate.…”
Section: Origin Of Secondary Carbonatesmentioning
confidence: 94%
“…Currently in the Yucatan Peninsula there are a variety of historical constructions and archeological sites built with stones. The Peninsula of Yucatan is a smooth carbonate platform developed from Cretaceous, Tertiary and Quaternary limestones, with predominantly shallow calcareous soil [1], containing different grain sizes, porosities, and texture. Also, many modern buildings use limestone as a primary construction material.…”
Section: Introductionmentioning
confidence: 99%
“…The year rainfall is in average 1036.9 mm. The soil type is litosol/ rendzina, usually stony, highly alkaline, and with low content of organic matter (Cabadas et al, 2010).…”
Section: Establishment Of Pepper Genotypes In Fieldmentioning
confidence: 99%