Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.2113/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
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ISSN | 1012-0750 |
EISSN | 1996-8590 |
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 |
推荐引用方式 GB/T 7714 | 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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