Hot spring deposits on a cliff face: A case study from Jifei, Yunnan Province, China

• Published in: Sedimentary geology Vol. 302; pp. 1 - 28
• Main Authors: Jones, Brian, Peng, Xiaotong
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.04.2014
• Subjects: Aragonite; Calcite; China; Cliffs; Crystals; Dendritic structure; Efflorescent minerals; Hot-spring; Precipitates; Precipitation; Spring water; China, People's Rep., Yunnan Prov; Aragonite; Hot-spring; Calcite; China; Efflorescent minerals
• ISSN: 0037-0738; 1879-0968
• DOI: 10.1016/j.sedgeo.2013.12.009

A cliff face in the Jifei karst area, southwest China, is covered by a spectacular succession of precipitates that formed from the hot spring water that once flowed down its surface. This layered succession is formed of aragonite layers that are formed largely of “fountain dendrites”, calcite layers that are formed mostly of “cone dendrites”, and microlaminated layers that contain numerous microbes and extracellular polymeric substances (EPS). Many of the aragonite crystals are hollow due to preferential dissolution of their cores. The calcite cone dendrites are commonly covered with biofilms, reticulate Si–Mg coatings, and other precipitates. The microbial layers include dodecahedral calcite crystals and accessory minerals that include opal-A, amorphous Si–Mg coatings, trona, barite, potassium sulfate crystals, mirabillite, and gaylussite. Interpretation of the δ18O(calcite) and δ18O(aragonite) indicates precipitation from water with a temperature of 54 to 66°C. The active hot spring at the top of the cliff presently ejects water at a temperature of 65°C. Layers, 1mm to 6cm thick, record temporal changes in the fluids from which the precipitates formed. This succession is not, however, formed of recurring cycles that can be linked to diurnal or seasonal changes in the local climate. Indeed, it appears that the climatic contrast between the wet season and the dry season had little impact on precipitation from the spring waters that flowed down the cliff face. Integration of currently available evidence suggests that the primary driving force was aperiodic changes in the CO2 content of the spring waters because that seems to be the prime control on the saturation levels that underpinned precipitation of the calcite and aragonite as well as the dissolution of the aragonite. Such variations in the CO2 content of the spring water were probably due to changes that took place in the subterranean plumbing system of the spring.