Formation and stability of oxygen-rich bubbles that shape photosynthetic mats

被引:105
作者
Bosak, T. [1 ]
Bush, J. W. M. [2 ]
Flynn, M. R. [3 ]
Liang, B. [1 ]
Ono, S. [1 ]
Petroff, A. P. [1 ]
Sim, M. S. [1 ]
机构
[1] MIT, EAPS, Cambridge, MA 02139 USA
[2] MIT, Dept Appl Math, Cambridge, MA 02139 USA
[3] Univ Alberta, Dept Mech Engn, Edmonton, AB, Canada
关键词
INDUCED SEDIMENTARY STRUCTURES; BENTHIC MICROBIAL MATS; NOONDAY DOLOMITE; TUBE STRUCTURES; NATIONAL-PARK; DEATH-VALLEY; PHOTOSYNTHESIS; MICROELECTRODE; COMMUNITIES; CARBONATES;
D O I
10.1111/j.1472-4669.2009.00227.x
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Gas release in photic-zone microbialites can lead to preservable morphological biosignatures. Here, we investigate the formation and stability of oxygen-rich bubbles enmeshed by filamentous cyanobacteria. Sub-millimetric and millimetric bubbles can be stable for weeks and even months. During this time, lithifying organic-rich laminae surrounding the bubbles can preserve the shape of bubbles. Cm-scale unstable bubbles support the growth of centimetric tubular towers with distinctly laminated mineralized walls. In environments that enable high photosynthetic rates, only small stable bubbles will be enclosed by a dense microbial mesh, while in deep waters extensive microbial mesh will cover even larger photosynthetic bubbles, increasing their preservation potential. Stable photosynthetic bubbles may be preserved as sub-millimeter and millimeter-diameter features with nearly circular cross-sections in the crests of some Proterozoic conical stromatolites, while centrimetric tubes formed around unstable bubbles provide a model for the formation of tubular carbonate microbialites that are not markedly depleted in 13C.
引用
收藏
页码:45 / 55
页数:11
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