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Li, C.-F.; Lin, Jian; Kulhanek, Denise K.; Williams, T.; Bao, Rui; Briais, A.; Brown, Elizabeth; Chen, Y.; Clift, Peter D.; Colwell, Frederick S.; Dadd, K.A.; Ding, Weiwei; Hernández‐Almeida, Iván; Huang, Xiaoxia; Hyun, Sangmin; Jiang, Tao; Koppers, A. A.; Li, Q.; Liu, C.; Liu, Q.; Liu, Z.; Nagai, Renata Hanae; Peleo-Alampay, A.; Su, Xinming; Sun, Zhen; Tejada, M. L. G.; Trinh, H.S.; Yeh, Yun-Chi; Zhang, C.; Zhang, F.; Zhang, G.-L.; Zhao, Xixi

doi:10.14379/iodp.proc.349.106.2015

Cited by 1 publication

(1 citation statement)

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“…Note also the dark, sometimes tufted, laminae (blue arrows) that envelop multiple vesicles. ( b ) Photomicrograph from a Miocene volcanoclastic sediment from the South China Sea showing devitrified basaltic volcanic glass (gl) with vesicles now infilled with carbonate (carb); image reproduced with permission from Li et al ( 2015 ). ( c – d ) Microstructures from the Dresser Formation whose morphologies are analogous to the fragment of Miocene vesicular devitrified volcanic glass in (b).…”

Section: Resultsmentioning

confidence: 99%

Volcanogenic Pseudo-Fossils from the ∼3.48 Ga Dresser Formation, Pilbara, Western Australia

et al. 2018

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The ∼3.48 billion-year-old Dresser Formation, Pilbara Craton, Western Australia, is a key geological unit for the study of Earth's earliest life and the habitats it occupied. Here, we describe a new suite of spheroidal to lenticular microstructures that morphologically resemble some previously reported Archean microfossils. Correlative microscopy shows that these objects have a size distribution, wall ultrastructure, and chemistry that are incompatible with a microfossil origin and instead are interpreted as pyritized and silicified fragments of vesicular volcanic glass. Organic kerogenous material is associated with much of the altered volcanic glass; variable quantities of organic carbon line or fill the insides of some individual vesicles, while relatively large, tufted organic-rich laminae envelop multiple vesicles.The microstructures reported herein constitute a new type of abiogenic artifact (pseudo-fossil) that must be considered when evaluating potential signs of early life on Earth or elsewhere. In the sample studied here, where hundreds of these microstructures are present, the combined evidence permits a relatively straightforward interpretation as vesicular volcanic glass. However, reworked, isolated, and silicified microstructures of this type may prove particularly problematic in early or extraterrestrial life studies since they adsorb carbon onto their surfaces and are readily pyritized, mimicking a common preservation mechanism for bona fide microfossils. In those cases, nanoscale analysis of wall ultrastructure would be required to firmly exclude a biological origin. Key Words: Microfossils—Pseudo-fossils—Volcanic vesicles—Archean life—Pilbara Craton—Dresser Formation. Astrobiology 18, 539–555.

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Section: Resultsmentioning

confidence: 99%