Arid
DOI10.1016/j.palaeo.2019.109266
Paleoproterozoic (ca. 1.9 Ga) megascopic life on land in Western Australia
Retallack, Gregory J.1; Mao, Xuegang2
通讯作者Retallack, Gregory J.
来源期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
EISSN1872-616X
出版年2019
卷号532
英文摘要Controversial hairpin-shaped trace fossils (Myxomitodes stirlingensis) and discoid fossils (Cyclomedusa davidi) are here reinterpreted in a reassessment of sedimentology and paleosols of the 1.9 +/- 0.1 Ga Stirling Range Formation of Western Australia. Paleosols in the Stirling Range Formation were recognized from complex cracking patterns (peds and cutans), chemical and mineralogical zonation (soil horizons), and poikiloblastic crystals (desert roses). Redox profiles of the paleosols are evidence of well-drained profiles of a coastal plain under a low oxygen (433 +/- 116 ppmv) and carbon dioxide (564 +/- 64 ppmv) atmosphere. Gypsum pseudo morphs in paleosols that are deeply weathered chemically, represent a persistence of acid sulfate weathering, better known in Archean paleosols before the Great Oxidation event at 2.45 Ga. Chemical composition of the paleosols is evidence of a humid (1478 +/- 182 mm mean annual precipitation) temperate (11.3 +/- 0.5 degrees C mean annual temperature) paleoclimate. Their paleoenvironmental setting was a coastal plain on a passive tectonic margin. Megafossils were found on paleosols of western red sandstones of the Stirling Range Formation, not in gray shales and sandstones of marine facies to the east. Trace fossils (Myxomitodes stirlingensis) and discoid fossils are both found at the surface of well drained paleosols, and so were not metazoan trails, nor sea jellies. Myxomitodes was more likely a grex (slug) trail of soil slime molds, and the Cyclomedusa discoids, were probably microbial colonies. Pervasive microfilamentous structures in the paleosol surface are additional evidence of Paleoproterozoic microbial earth ecosystems.
英文关键词Stirling Range Formation Paleosol Paleoclimate Mycetozoa Microbial earth
类型Article
语种英语
国家USA ; Peoples R China
收录类别SCI-E
WOS记录号WOS:000484871600012
WOS关键词ALBANY-FRASER OROGEN ; STIRLING RANGE FORMATION ; RARE-EARTH-ELEMENTS ; PRECAMBRIAN PALEOSOLS ; GREENSTONE-BELT ; IRON-FORMATION ; CAMBRIAN PALEOSOLS ; PILBARA CRATON ; MASS-BALANCE ; MOBILE BELT
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS研究方向Physical Geography ; Geology ; Paleontology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/217870
作者单位1.Univ Oregon, Dept Earth Sci, Eugene, OR 97403 USA;
2.Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China
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Retallack, Gregory J.,Mao, Xuegang. Paleoproterozoic (ca. 1.9 Ga) megascopic life on land in Western Australia[J],2019,532.
APA Retallack, Gregory J.,&Mao, Xuegang.(2019).Paleoproterozoic (ca. 1.9 Ga) megascopic life on land in Western Australia.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,532.
MLA Retallack, Gregory J.,et al."Paleoproterozoic (ca. 1.9 Ga) megascopic life on land in Western Australia".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 532(2019).
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