Arid
DOI10.2113/gssajg.119.3.495
Geological constraints on Archean (3.22 Ga) coastal -zone processes from the Dycedale Syncline, Barberton Greenstone Belt
Heubeck, C.1; Blaesing, S.2; Grund, M.2; Drabon, N.3; Homann, M.2,4; Nabhan, S.2,5
通讯作者Heubeck, C.
来源期刊SOUTH AFRICAN JOURNAL OF GEOLOGY
ISSN1012-0750
EISSN1996-8590
出版年2016
卷号119期号:3页码:495-518
英文摘要

Geological constraints bearing on Paleoarchean surface environments are rare but critical, establishing the physiological consequences of a very different physical environment for early life, including a different tectonic style, closer Earth-Moon interaction, different chemical composition of atmosphere and hydrosphere, higher weathering intensity, and to validate geochemical proxy data. Strata relevant to these topics can he studied in uniquely accessible, subvertically dipping beds of the Moodies Group (ca. 3.22 Ga) within the tightly folded, steeply plunging western Dycedale Syncline of the Barberton Greenstone Belt. They display a large variety of environment specific sedimentary structures in a small (ca. 1 km(2)) but excellently exposed area, including microbial mats, abundant shoreline and tidal structures and early diagenetic pedogenic nodules. These are set among conglomerates, sandstones, minor lava flows and banded-iron formation within an initially deepening-, then shallowing-upward sequence, including (from base to top) braided-fluvial floodplain, sandy shoreline, and estuarine and protected tidal environments, some of which were temporally choked by volcanic ash. Shorelines were (semi-)arid, had fluctuating groundwater levels and moderate to high tides. Nevertheless, diverse microbial communities gained footholds in this challenging setting, including sulfate reducers in the shallow subsurface, photosynthesizers along high-energy shorelines, and photoferrotrophs or other Fe-metabolizing chemolithautotrophs in lagoonal or offshore settings.


Facies analysis and regional structural geology suggest that the Dycedale area formed a minor, structurally controlled basin within a southward-facing fold-and-thrust belt which became intensely deformed during subsequent steepening. Overall, the datasets derived from this area allow the detailed description of interactions between early Earth’s volcanism, atmo- and hydrosphere and place the emergent biosphere into physical settings that are observable to such detail in only few other places worldwide.


类型Article
语种英语
国家Germany ; USA ; France
收录类别SCI-E
WOS记录号WOS:000400728100003
WOS关键词ARCHAEAN MOODIES GROUP ; FIG TREE GROUPS ; SOUTH-AFRICA ; MICROBIAL MATS ; MOUNTAIN LAND ; SEDIMENTARY STRUCTURES ; TIDAL RHYTHMITES ; TRANSITION ; TECTONICS ; EVOLUTION
WOS类目Geology
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/196523
作者单位1.Friedrich Schiller Univ Jena, Burgweg 11, D-07749 Jena, Germany;
2.Free Univ Berlin, Inst Geol Wissensch, D-12249 Berlin, Germany;
3.Stanford Univ, Dept Geosci, Stanford, CA 94305 USA;
4.Inst Univ Europeen Mer, F-29280 Plouzane, France;
5.Univ Jena, Inst Geowissensch, D-07749 Jena, Germany
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Heubeck, C.,Blaesing, S.,Grund, M.,et al. Geological constraints on Archean (3.22 Ga) coastal -zone processes from the Dycedale Syncline, Barberton Greenstone Belt[J],2016,119(3):495-518.
APA Heubeck, C.,Blaesing, S.,Grund, M.,Drabon, N.,Homann, M.,&Nabhan, S..(2016).Geological constraints on Archean (3.22 Ga) coastal -zone processes from the Dycedale Syncline, Barberton Greenstone Belt.SOUTH AFRICAN JOURNAL OF GEOLOGY,119(3),495-518.
MLA Heubeck, C.,et al."Geological constraints on Archean (3.22 Ga) coastal -zone processes from the Dycedale Syncline, Barberton Greenstone Belt".SOUTH AFRICAN JOURNAL OF GEOLOGY 119.3(2016):495-518.
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