BIOGENICITY AND CHARACTERIZATION OF MOONMILK IN THE GROTTA NERA (MAJELLA NATIONAL PARK, ABRUZZI, CENTRAL ITALY)

被引:25
作者
Cacchio, Paola [1 ]
Ferrini, Gianluca [2 ]
Ercole, Claudia [1 ]
Del Gallo, Maddalena [1 ]
Lepidi, Aldo [1 ]
机构
[1] Univ Aquila, Dept Life Hlth & Environm Sci, Microbiol Lab, I-67010 Laquila, Italy
[2] Univ Aquila, Dept Life Hlth & Environm Sci, Geol Lab, I-67010 Laquila, Italy
关键词
CALCIUM-CARBONATE PRECIPITATION; DISSOLVED ORGANIC-MATTER; MICROBIAL COMMUNITY; CAVE ENVIRONMENTS; DRIPPING WATERS; BACTERIA; INVOLVEMENT; ORIGIN; GEOMICROBIOLOGY; SPELEOTHEMS;
D O I
10.4311/2012MB0275
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Observations and hypotheses on the possible influence of unidentified calcifying bacteria on moonmilk speleothem formation in the Grotta Nera are reported for the first time. The Majella Massif hosts a complex karst system of several caves; the accessible Grotta Nera is the most interesting one. Despite its name, the cave is characterized by particularly abundant ivory-white deposits of moonmilk. Two samples of moonmilk were analyzed to determine the geochemistry, fabric, depositional setting, and extent of biogenicity. For this, we combined geochemical, scanning electron microscopic, microbiological, and in vitro precipitation studies. X-ray diffraction of the moonmilk deposits gave clear evidence for the presence of calcite. Scanning electron microscopy showed that moonmilk in the Grotta Nera consists of a network of calcite fibers oriented in all directions, resembling a felted mat. The cultivation on specific medium of moonmilk and drip-water samples showed the presence of fungi, actinomycetes, and other bacteria, but the dominant cultivable microorganisms were bacteria, which produced significant crystallization. Examination of Gram-stained smears taken from the fifteen different colony types showed that the majority (66.7%) of the bacterial isolates were Gram-negative. Single small rods and rod chains were the most common bacteria isolated from the Grotta Nera. None of the molds isolated from the Grotta Nera samples were able to precipitate CaCO3 crystals, suggesting a major bacterial contribution to moonmilk deposition in the cave. Bacteria were capable of precipitating CaCO3 on B-4 solid medium at 15 (cave temperature), 22, and 32 degrees C. The calcifying bacteria isolated from the Grotta Nera showed a greater capability to solubilize CaCO3 than those associated with consolidated stalactites sampled from previously studied caves. The electron microscopy and microbiological evidences, together with the geochemistry and environmental data, allowed us to postulate the biogenic nature of the moonmilk in the Grotta Nera Cave.
引用
收藏
页码:88 / 103
页数:16
相关论文
共 76 条
[71]   Thermally assisted hydrolysis and methylation of dissolved organic matter in dripping waters from the Altamira Cave [J].
Saiz-Jimenez, C ;
Hermosin, B .
JOURNAL OF ANALYTICAL AND APPLIED PYROLYSIS, 1999, 49 (1-2) :337-347
[72]  
Savini N., 2004, GROTTE MONTAGNA SACR
[73]  
Schlegel H.G., 1993, General Microbiology
[74]   Shifts in the microbial community in rhizosphere and non-rhizosphere soils during the growth of Agrostis stolonifera [J].
Steer, J ;
Harris, JA .
SOIL BIOLOGY & BIOCHEMISTRY, 2000, 32 (06) :869-878
[75]  
Sweeting MarjorieMary., 1973, Karst Landforms
[76]  
Vezzani L., 1993, CARTA GEOLOGICA ABRU