-This paper presents the results of a taphonomic study of Holocene diatoms in the Llano Grande Basin, PĂĄramo de Frontino, which is located 3,460 m above sea level in the northwestern Andean Cordillera (6Âș29'N/76Âș6'W), Colombia. Samples measuring 1 cm 3 from 57 levels distributed over a core depth of 8.5 m (LLG3) were randomly collected from sediment representing a paleolake that developed on the Llano Grande Basin. The density of diatoms and the number of fragmented and dissolved valves were estimated from 10 ÎŒL of each sample. A high variability in the density and preservation of the diatom assemblages was verifi ed along the core, which is related to temperature variation, macroinvertebrates grazing, volcanic ash infl ux, and water-level fl uctuations over the 11.000 C 14 years BP. Fragmentation was higher than dissolution, which indicates the predominance of lotic environments and grazing. The substantial decrease in the diatoms on specifi c level is interpreted as a result of the limitation of silica, decreased water levels, intense herbivory, dry environment or dissolution. In these cases, it is impossible to recognize most of the periphytic diatoms due to the high degree of fragmentation of the frustules. The authors conclude that the high degree of variation of the taphonomic damage in the diatoms of PĂĄramo de Frontino represents different environmental events along the Holocene. Therefore, in the early Holocene, input from ash and high temperatures favored reproduction, which resulted in the high density of diatoms. In the last 4,000 years, the water level in the lake has decreased, and probably the predation on diatoms has increased as evidenced by the increasing of fragmentation of the state 3.Key words: taphonomy, diatom paleoecology, peats, Holocene.RESUMO -Este trabalho apresenta os resultados do estudo tafonĂŽmico das diatomĂĄceas holocĂȘnicas da Bacia Llano Grande, PĂĄramo de Frontino, localizado a 3.460 m acima do nĂvel do mar, noroeste da Cordilheira dos Andes (6°29'N/76°6'O), ColĂŽmbia. Foram coletadas aleatoriamente amostras de 1 cm 3 de sedimentos, distribuĂdas em 57 nĂveis ao longo dos 8,5 m do testemunho LLG3, as quais representam um paleolago que se desenvolveu na bacia. A densidade das diatomĂĄceas e o nĂșmero de valvas fragmentadas e dissolvidas foram estimados a partir de 10 uL de cada amostra. A alta variabilidade na densidade e preservação das assembleias de diatomĂĄceas no testemunho estĂĄ relacionada com variação de temperatura, consumo por macroinvertebrados, aporte de cinzas vulcĂąnicas e fl utuaçÔes no nĂvel de ĂĄgua ao longo dos 11.000 anos AP (C 14 ). A fragmentação foi superior Ă dissolução, o que indica predominĂąncia de ambientes lĂłticos e consumo por herbĂvoros. O decrĂ©scimo substancial das diatomĂĄceas em nĂvel especĂfi co Ă© interpretado como resultado da limitação de sĂlica, diminuição dos nĂveis de ĂĄgua, intensa herbivoria, ambiente seco ou dissolução. Nestes casos, Ă© impossĂvel reconhecer a maioria das diatomĂĄceas perifĂticas devido ao grau de fragmentação das frĂșstulas...