Ancient microbial activity recorded in fracture fillings from granitic rocks (Äspö Hard Rock Laboratory, Sweden)

Year:

2012

Type of Publication:

Artikel

Autoren:

HEIM, C.; LAUSMAA, J.; SJÖVALL, P.; TOPORSKI, J.; DIEING, T.; Simon, Klaus; HANSEN, B. T.; Kronz, Andreas; ARP, G.; REITNER, J.; THIEL, V.

Journal:

Geobiology

Volume:

10

Nummer:

4

Seiten:

280-297

ISSN:

1472-4669

BibTex:

@article{GBI:GBI328, author = "C. HEIM and J. LAUSMAA and P. SJ{\"O}VALL and J. TOPORSKI and T. DIEING and Klaus Simon and B. T. HANSEN and Andreas Kronz and G. ARP and J. REITNER and V. THIEL", abstract = "Fracture minerals within the 1.8-Ga-old {\"A}sp{\"o} Diorite (Sweden) were investigated for fossil traces of subterranean microbial activity. To track the potential organic and inorganic biosignatures, an approach combining complementary analytical techniques of high lateral resolution was applied to drill core material obtained at −450 m depth in the {\"A}sp{\"o} Hard Rock Laboratory. This approach included polarization microscopy, time-of-flight secondary ion mass spectrometry (ToF-SIMS), confocal Raman microscopy, electron microprobe (EMP) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The fracture mineral succession, consisting of fluorite and low-temperature calcite, showed a thin (20–100 μm), dark amorphous layer lining the boundary between the two phases. Microscopic investigations of the amorphous layer revealed corrosion marks and, in places, branched tubular structures within the fluorite. Geochemical analysis showed significant accumulations of Si, Al, Mg, Fe and the light rare earth elements (REE) in the amorphous layer. In the same area, ToF-SIMS imaging revealed abundant, partly functionalized organic moieties, for example, CxHy+, CxHyN+, CxHyO+. The presence of such functionalized organic compounds was corroborated by Raman imaging showing bands characteristic of C-C, C-N and C-O bonds. According to its organic nature and the abundance of relatively unstable N- and O- heterocompounds, the organic-rich amorphous layer is interpreted to represent the remains of a microbial biofilm that established much later than the initial cooling of the Precambrian host rock. Indeed, δ13C, δ18O and 87Sr/86Sr isotope data of the fracture minerals and the host rock point to an association with a fracture reactivation event in the most recent geological past.", doi = "10.1111/j.1472-4669.2012.00328.x", issn = "1472-4669", journal = "Geobiology", number = "4", pages = "280--297", publisher = "Blackwell Publishing Ltd", title = "{A}ncient microbial activity recorded in fracture fillings from granitic rocks ({\"{A}}sp{\"o} {H}ard {R}ock {L}aboratory, {S}weden)", url = "http://dx.doi.org/10.1111/j.1472-4669.2012.00328.x", volume = "10", year = "2012", }

Kurzzusammenfassung:

Fracture minerals within the 1.8-Ga-old Äspö Diorite (Sweden) were investigated for fossil traces of subterranean microbial activity. To track the potential organic and inorganic biosignatures, an approach combining complementary analytical techniques of high lateral resolution was applied to drill core material obtained at −450 m depth in the Äspö Hard Rock Laboratory. This approach included polarization microscopy, time-of-flight secondary ion mass spectrometry (ToF-SIMS), confocal Raman microscopy, electron microprobe (EMP) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The fracture mineral succession, consisting of fluorite and low-temperature calcite, showed a thin (20–100 μm), dark amorphous layer lining the boundary between the two phases. Microscopic investigations of the amorphous layer revealed corrosion marks and, in places, branched tubular structures within the fluorite. Geochemical analysis showed significant accumulations of Si, Al, Mg, Fe and the light rare earth elements (REE) in the amorphous layer. In the same area, ToF-SIMS imaging revealed abundant, partly functionalized organic moieties, for example, CxHy+, CxHyN+, CxHyO+. The presence of such functionalized organic compounds was corroborated by Raman imaging showing bands characteristic of C-C, C-N and C-O bonds. According to its organic nature and the abundance of relatively unstable N- and O- heterocompounds, the organic-rich amorphous layer is interpreted to represent the remains of a microbial biofilm that established much later than the initial cooling of the Precambrian host rock. Indeed, δ13C, δ18O and 87Sr/86Sr isotope data of the fracture minerals and the host rock point to an association with a fracture reactivation event in the most recent geological past.