Cyanobacteria evolution: Insight from the fossil record

被引:135
作者
Demoulin, Catherine F. [1 ]
Lara, Yannick J. [1 ]
Cornet, Luc [1 ,2 ]
Francois, Camille [1 ]
Baurain, Denis [2 ]
Wilmotte, Annick [3 ]
Javaux, Emmanuelle J. [1 ]
机构
[1] Univ Liege, UR Astrobiol, Dept Geol, Early Life Traces & Evolut Astrobiol, Liege, Belgium
[2] Univ Liege, Eukaryot Phylogen, InBioS PhytoSYST, Liege, Belgium
[3] Univ Liege, Ctr Prot Engn, BCCM ULC Cyanobacteria Collect, InBioS CIP, Liege, Belgium
基金
欧洲研究理事会;
关键词
Biosignatures; Cyanobacteria; Evolution; Microfossils; Molecular clocks; Precambrian; ORGANIC-WALLED MICROFOSSILS; BLUE-GREEN-ALGAE; GA APEX CHERT; OXYGENIC PHOTOSYNTHESIS; ANOXYGENIC PHOTOSYNTHESIS; GAOYUZHUANG FORMATION; BELCHER ISLANDS; MCARTHUR GROUP; MICRO-FOSSILS; SEMRI GROUP;
D O I
10.1016/j.freeradbiomed.2019.05.007
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
Cyanobacteria played an important role in the evolution of Early Earth and the biosphere. They are responsible for the oxygenation of the atmosphere and oceans since the Great Oxidation Event around 2.4 Ga, debatably earlier. They are also major primary producers in past and present oceans, and the ancestors of the chloroplast. Nevertheless, the identification of cyanobacteria in the early fossil record remains ambiguous because the morphological criteria commonly used are not always reliable for microfossil interpretation. Recently, new biosignatures specific to cyanobacteria were proposed. Here, we review the classic and new cyanobacterial biosignatures. We also assess the reliability of the previously described cyanobacteria fossil record and the challenges of molecular approaches on modern cyanobacteria. Finally, we suggest possible new calibration points for molecular clocks, and strategies to improve our understanding of the timing and pattern of the evolution of cyanobacteria and oxygenic photosynthesis.
引用
收藏
页码:206 / 223
页数:18
相关论文
共 261 条
[111]  
2
[112]  
Kaplan-Levy RN, 2010, TOP CURR GENET, V21, P5, DOI 10.1007/978-3-642-12422-8_2
[113]   What caused the rise of atmospheric O2? [J].
Kasting, James F. .
CHEMICAL GEOLOGY, 2013, 362 :13-25
[114]   Cyanobacteria in Sulfidic Spring Microbial Mats Can Perform Oxygenic and Anoxygenic Photosynthesis Simultaneously during an Entire Diurnal Period [J].
Klatt, Judith M. ;
de Beer, Dirk ;
Haeusler, Stefan ;
Polerecky, Lubos .
FRONTIERS IN MICROBIOLOGY, 2016, 7
[115]   FILAMENTOUS MICROFOSSILS IN THE EARLY PROTEROZOIC TRANSVAAL SUPERGROUP - THEIR MORPHOLOGY, SIGNIFICANCE, AND PALEOENVIRONMENTAL SETTING [J].
KLEIN, C ;
BEUKES, NJ ;
SCHOPF, JW .
PRECAMBRIAN RESEARCH, 1987, 36 (01) :81-94
[116]  
Knoll A.H., 1992, Early Organic Evolution: Implications for mineral and energy resources, P450, DOI DOI 10.1007/978-3-642-76884-2_35
[117]   PALEOENVIRONMENTAL DISTRIBUTION OF MICROFOSSILS AND STROMATOLITES IN THE UPPER PROTEROZOIC BACKLUNDTOPPEN FORMATION, SPITSBERGEN [J].
KNOLL, AH ;
SWETT, K ;
BURKHARDT, E .
JOURNAL OF PALEONTOLOGY, 1989, 63 (02) :129-145
[118]   PALEOBIOLOGY OF A NEOPROTEROZOIC TIDAL FLAT LAGOONAL COMPLEX - THE DRAKEN CONGLOMERATE FORMATION, SPITSBERGEN [J].
KNOLL, AH ;
SWETT, K ;
MARK, J .
JOURNAL OF PALEONTOLOGY, 1991, 65 (04) :531-570
[119]   ANATOMY AND TAPHONOMY OF A PRECAMBRIAN ALGAL STROMATOLITE [J].
KNOLL, AH ;
GOLUBIC, S .
PRECAMBRIAN RESEARCH, 1979, 10 (1-2) :115-151
[120]   DISTRIBUTION AND DIAGENESIS OF MICROFOSSILS FROM THE LOWER PROTEROZOIC DUCK CREEK DOLOMITE, WESTERN-AUSTRALIA [J].
KNOLL, AH ;
STROTHER, PK ;
ROSSI, S .
PRECAMBRIAN RESEARCH, 1988, 38 (03) :257-279