globalchange  > 气候变化事实与影响
DOI: 10.1111/gbi.12327
WOS记录号: WOS:000458929400007
论文题名:
Mineralized microbialites as archives of environmental evolution, Laguna Negra, Catamarca Province, Argentina
作者: Buongiorno, Joy1; Gomez, Fernando J.2; Fike, David A.3; Kah, Linda C.4
通讯作者: Buongiorno, Joy
刊名: GEOBIOLOGY
ISSN: 1472-4677
EISSN: 1472-4669
出版年: 2019
卷: 17, 期:2, 页码:199-222
语种: 英语
WOS关键词: ORGANIC-MATTER ; CARBONATE PRECIPITATION ; CHILEAN ALTIPLANO ; ATACAMA-ALTIPLANO ; ISOTOPIC COMPOSITION ; CALCIUM-CARBONATE ; ANDEAN ALTIPLANO ; HYPERSALINE LAKE ; STABLE-ISOTOPE ; CLIMATE-CHANGE
WOS学科分类: Biology ; Environmental Sciences ; Geosciences, Multidisciplinary
WOS研究方向: Life Sciences & Biomedicine - Other Topics ; Environmental Sciences & Ecology ; Geology
英文摘要:

Environmental fluctuations are recorded in a variety of sedimentary archives of lacustrine depositional systems. Geochemical signals recovered from bottom sediments in closed-basin lakes are among the most sensitive paleoenvironmental indicators and are commonly used in reconstructing lake evolution. Microbialites (i.e., organosedimentary deposits accreted through microbial trapping and binding of detrital sediment or in situ mineral precipitation on organics [Palaios, 2, 1987, 241]), however, have been largely overlooked as paleoenvironmental repositories. Here, we investigate concentrically laminated mineralized microbialites from Laguna Negra, a high-altitude (4,100 m above sea level) hypersaline, closed-basin lake in northwestern Argentina, and explore the potential for recovery of environmental signals from these unique sedimentary archives. Spatial heterogeneity in hydrological regime helps define zones inside Laguna Negra, each with their own morphologically distinct microbialite type. Most notably, platey microbialites (in Zone 3A) are precipitated by evaporative concentration processes, while discoidal oncolites (in Zone 3C) are interpreted result from fluid mixing and biologically mediated nucleation. This spatial heterogeneity is reflected in petrographically distinct carbonate fabrics: micritic, botryoidal, and isopachous. Fabric type is interpreted to reflect a combination of physical and biological influences during mineralization, and paired C-isotope measurement of carbonate and organic matter supports ecological differences as a dominant control on C-isotopic evolution between zones. Laminae of Laguna Negra microbialites preserve a range of delta C-13(carb) from +5.75 parts per thousand to +18.25 parts per thousand and delta O-18(carb) from -2.04 parts per thousand to +9.28 parts per thousand. Temporal trends of lower carbon and oxygen isotopic compositions suggest that the influence of CO2 degassing associated with evaporation has decreased over time. Combined, these results indicate that microbialite archives can provide data that aid in interpretation of both lake paleohydrology and paleoenvironmental change.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/131400
Appears in Collections:气候变化事实与影响

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作者单位: 1.Univ Tennessee, Dept Microbiol, Knoxville, TN 37996 USA
2.CONICET Cordoba, Ctr Invest Ciencias Tierra Cordoba, Cordoba, Argentina
3.Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA
4.Univ Tennessee, Dept Earth & Planetary Sci, Knoxville, TN USA

Recommended Citation:
Buongiorno, Joy,Gomez, Fernando J.,Fike, David A.,et al. Mineralized microbialites as archives of environmental evolution, Laguna Negra, Catamarca Province, Argentina[J]. GEOBIOLOGY,2019-01-01,17(2):199-222
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