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Matground structures and redox facies

https://doi.org/10.2307/3515359
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inferred← citeshttps://doi.org/10.2139/ssrn.4679511openalex-extracted
Implicaciones De Los Registros Microbianos En La Formación La Chilca (Hirnantiense - Wenlock), Precordillera Central, San Juan Argentina
inferred← citeshttps://doi.org/10.1002/gj.1165openalex-snapshot
Process regime change on a Silurian siliciclastic shelf: controlling influences on deposition of the Gray Sandstone Formation, Pembrokeshire, UK
inferred← citeshttps://doi.org/10.1002/gj.3312openalex-snapshot
Flat pebbles and their edge‐wise fabric in relation to 2‐D microbial mat
inferred← citeshttps://doi.org/10.1002/gj.3390openalex-snapshot
Stratigraphy and facies analysis of the L a C hilca F ormation, C entral P recordillera: Insights on the postglacial O rdovician– S ilurian boundary and Early S ilurian deposits from A rgentina
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From Fossils to Astrobiology
inferred← citeshttps://doi.org/10.1007/978-1-4020-8837-7_9openalex-snapshot
Cyanobacterial Mat Features Preserved in the Siliciclastic Sedimentary Record
inferred← citeshttps://doi.org/10.1007/978-1-4020-9053-0_9openalex-snapshot
Use of Event Beds and Sedimentary Cycles in High-Resolution Stratigraphic Correlation of Lithologically Repetitive Successions
inferred← citeshttps://doi.org/10.1007/978-1-4020-9212-1_148openalex-snapshot
Mat-Related Sedimentary Structures
inferred← citeshttps://doi.org/10.1007/978-3-540-47226-1_12openalex-snapshot
Pseudo-Traces
inferred← citeshttps://doi.org/10.1007/978-3-642-10415-2_29openalex-snapshot
Sedimentology and Palaeoecology of Ernietta-Bearing Ediacaran Deposits in Southern Namibia: Implications for Infaunal Vendobiont Communities
inferred← citeshttps://doi.org/10.1007/978-3-662-44185-5_1004openalex-snapshot
Microbially Induced Sedimentary Structures
inferred← citeshttps://doi.org/10.1007/978-90-481-3428-1_22openalex-snapshot
The Late Middle Devonian (Givetian) Global Taghanic Biocrisis in Its Type Area (Northern Appalachian Basin): Geologically Rapid Faunal Transitions Driven by Global and Local Environmental Changes
inferred← citeshttps://doi.org/10.1007/978-90-481-3799-2_5openalex-snapshot
Paleoenvironmental Context of Microbial Mat-Related Structures in Siliciclastic Rocks
inferred← citeshttps://doi.org/10.1007/978-90-481-3799-2_6openalex-snapshot
Microbially Related Structures in Siliciclastic Sediment Resembling Ediacaran Fossils: Examples from India, Ancient and Modern
inferred← citeshttps://doi.org/10.1007/978-94-017-0193-8_12openalex-snapshot
Biofilms and Macroorganisms
inferred← citeshttps://doi.org/10.1007/978-94-017-0193-8_18openalex-snapshot
The Role of Biofilms in the Fossilization of Non-Biomineralized Tissues
inferred← citeshttps://doi.org/10.1007/978-981-32-9551-3_5openalex-snapshot
Microbial Mat Structures Formed Within Siliciclastics
inferred← citeshttps://doi.org/10.1007/978-981-99-6936-4_16openalex-snapshot
Stratigraphy and Sedimentology of the Proterozoic at the Jixian Section, Tianjin
inferred← citeshttps://doi.org/10.1007/bf02703025openalex-snapshot
Microbial mat-induced sedimentary structures in siliciclastic sediments: Examples from the 1.6 Ga Chorhat Sandstone, Vindhyan Supergroup, M.P., India
inferred← citeshttps://doi.org/10.1007/bf02703026openalex-snapshot
Petrographic observations suggestive of microbial mats from Rampur Shale and Bijaigarh Shale, Vindhyan basin, India
inferred← citeshttps://doi.org/10.1007/bf03043868openalex-snapshot
Bio-sedimentary structures evolving from the interaction of microbial mats, burrowing beetles and the physical environment of Tunisian coastal sabkhas
inferred← citeshttps://doi.org/10.1007/s10347-012-0331-3openalex-snapshot
Facies control on lower Cambrian wrinkle structure development and paleoenvironmental distribution, southern Great Basin, United States
inferred← citeshttps://doi.org/10.1007/s10347-013-0379-8openalex-snapshot
Microbial and physical sedimentary structures in modern evaporitic coastal environments of Saudi Arabia and Egypt
inferred← citeshttps://doi.org/10.1007/s10347-014-0400-xopenalex-snapshot
Suspected microbial-induced sedimentary structures (MISS) in Furongian (Upper Cambrian; Jiangshanian, Sunwaptan) strata of the Upper Mississippi Valley
inferred← citeshttps://doi.org/10.1007/s12040-020-01416-xopenalex-snapshot
Implications of microbial mat induced sedimentary structures (MISS) in carbonate rocks: An insight from Proterozoic Rohtas Limestone and Bhander Limestone, India
inferred← citeshttps://doi.org/10.1007/s12040-024-02503-zopenalex-snapshot
Psammichnites gigas gigas sub-ichnozone and microbially induced sedimentary structures (MISS) from Kunzam La Formation (Cambrian), Hojis Valley, Kinnaur, Himachal Himalaya
inferred← citeshttps://doi.org/10.1007/s40010-013-0088-2openalex-snapshot
Facies-Dependent Occurrence of Shrinkage Cracks in the Glauconitic Sandstone, Semri Group, Vindhyan Supergroup
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01310-3openalex-snapshot
Oxygen and Early Animal Evolution
inferred← citeshttps://doi.org/10.1016/b978-0-323-95547-8.00034-3openalex-snapshot
Microbial mats in the siliciclastic rock record
inferred← citeshttps://doi.org/10.1016/j.earscirev.2006.12.001openalex-snapshot
Wrinkle structures—a critical review
inferred← citeshttps://doi.org/10.1016/j.earscirev.2008.08.002openalex-snapshot
The criteria for the biogeneicity of microbially induced sedimentary structures (MISS) in Archean and younger, sandy deposits
inferred← citeshttps://doi.org/10.1016/j.earscirev.2009.06.001openalex-snapshot
The paleoenvironmental distribution of Phanerozoic wrinkle structures
inferred← citeshttps://doi.org/10.1016/j.earscirev.2009.07.002openalex-snapshot
Remarkable preservation of microbial mats in Neoproterozoic siliciclastic settings: Implications for Ediacaran taphonomic models
inferred← citeshttps://doi.org/10.1016/j.earscirev.2009.11.002openalex-snapshot
Cambrian to Devonian evolution of alluvial systems: The sedimentological impact of the earliest land plants
inferred← citeshttps://doi.org/10.1016/j.earscirev.2016.01.005openalex-snapshot
Resolving MISS conceptions and misconceptions: A geological approach to sedimentary surface textures generated by microbial and abiotic processes
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.07.012openalex-snapshot
Unusual shallow marine matground-adapted benthic biofacies from the Lower Triassic of the northern Paleotethys: Implications for biotic recovery following the end-Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.104976openalex-snapshot
Biostabilization: Parameterizing the interactions between microorganisms and siliciclastic marine sediments
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103590openalex-snapshot
Reassessing Early Triassic wrinkle structures from moderate-high latitudes: An updated interpretation of metazoan colonization in matground ecosystems after the Permian-Triassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2007.03.004openalex-snapshot
Siliciclastic biolaminites indicative of widespread microbial mats in the Neoproterozoic Nama Group of Namibia
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2010.04.006openalex-snapshot
Evidence for participation of microbial mats in the deposition of the siliciclastic ‘ore formation’ in the Copperbelt of Zambia
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2021.104120openalex-snapshot
Environmental constraints on the distribution of matground and mixground ecosystems across the Cambrian Series 2–Miaolingian boundary interval in Iran: A case study for the central sector of northern Gondwana
inferred← citeshttps://doi.org/10.1016/j.jop.2016.05.001openalex-snapshot
Microbial mat-related structures shared by both siliciclastic and carbonate formations
inferred← citeshttps://doi.org/10.1016/j.jop.2025.04.001openalex-snapshot
Microbially induced sedimentary structures (MISS) from Paleoproterozoic siliciclastic successions and their bearing on shallow marine sedimentation: Bayana Basin, North Delhi Fold Belt, India
inferred← citeshttps://doi.org/10.1016/j.jsames.2021.103213openalex-snapshot
Dictyodora-Nereites dominated ichnofauna in the Silurian−Devonian turbidite-like deposits of central-western Gondwana (San Rafael Block, Argentina): New stratigraphic and bathymetric constraints
inferred← citeshttps://doi.org/10.1016/j.margeo.2013.10.002openalex-snapshot
Modern microbial mats in siliciclastic tidal flats: Evolution, structure and the role of hydrodynamics
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2010.11.002openalex-snapshot
Sedimentation patterns during the Precambrian: A unique record?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.12.013openalex-snapshot
Possible evidence for episodic epeiric marine and fluvial sedimentation (and implications for palaeoclimatic conditions), c. 2.3–1.8 Ga, Kaapvaal craton, South Africa
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.11.010openalex-snapshot
Genesis of unusual lithologies associated with the Late Middle Devonian Taghanic biocrisis in the type Taghanic succession of New York State and Pennsylvania
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.06.021openalex-snapshot
Microbially induced sedimentary structures in Neogene tidal flats from Argentina: Paleoenvironmental, stratigraphic and taphonomic implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.05.027openalex-snapshot
The middle Rhuddanian (lower Silurian) ‘hot’ shale of North Africa and Arabia: An atypical hydrocarbon source rock
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.06.013openalex-snapshot
Microbial mats in the terrestrial Lower Triassic of North China and implications for the Permian–Triassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109631openalex-snapshot
Paleobiology and taphonomy of exceptionally preserved organisms from the Waukesha Biota (Silurian), Wisconsin, USA
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114123openalex-snapshot
An exceptionally preserved Cambrian Psammichnites assemblage as a window into the earliest extensive horizontal-burrowing ecosystem engineers in shallow marine environments
inferred← citeshttps://doi.org/10.1016/j.precamres.2005.05.007openalex-snapshot
Suspected microbial mat-related crack-like sedimentary structures in the Palaeoproterozoic Magaliesberg Formation sandstones, South Africa
inferred← citeshttps://doi.org/10.1016/j.precamres.2006.01.003openalex-snapshot
Spatial and temporal distribution of microbially induced sedimentary structures: A case study from siliciclastic storm deposits of the 2.9Ga Witwatersrand Supergroup, South Africa
inferred← citeshttps://doi.org/10.1016/j.precamres.2007.07.019openalex-snapshot
Microbial mat mediated structures in the Ediacaran Sonia Sandstone, Rajasthan, India, and their implications for proterozoic sedimentation
inferred← citeshttps://doi.org/10.1016/j.precamres.2012.01.006openalex-snapshot
Exceptionally preserved microbially induced sedimentary structures from the Ediacaran post-glacial successions in the Kimberley region, northwestern Australia
inferred← citeshttps://doi.org/10.1016/j.precamres.2012.11.008openalex-snapshot
Proliferation of MISS-forming microbial mats after the late Neoproterozoic glaciations: Evidence from the Kimberley region, NW Australia
inferred← citeshttps://doi.org/10.1016/j.precamres.2013.08.001openalex-snapshot
Evidence for 2.0Ga continental microbial mats in a paleodesert setting
inferred← citeshttps://doi.org/10.1016/j.precamres.2016.05.010openalex-snapshot
Microbially induced sedimentary structures in the Paleoproterozoic, upper Huronian Supergroup, Canada
inferred← citeshttps://doi.org/10.1016/j.precamres.2021.106449openalex-snapshot
Descending into the “snowball”: High resolution sedimentological and geochemical analysis across the Tonian to Cryogenian boundary in South Australia
inferred← citeshttps://doi.org/10.1016/j.precamres.2023.107135openalex-snapshot
Microbially induced sedimentary structures from the Ediacaran of Anti-Atlas, Morocco
inferred← citeshttps://doi.org/10.1016/j.precamres.2023.107188openalex-snapshot
Fossils, pseudofossils and problematica from the Ura Formation: Ediacaran of the Patom Basin, Siberia
inferred← citeshttps://doi.org/10.1016/j.precamres.2025.107885openalex-snapshot
The Adoudou Biota: A new window on the Ediacaran-Cambrian transition from the western Anti-Atlas, Morocco
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2004.12.012openalex-snapshot
Microbial mat control on siliciclastic Precambrian sequence stratigraphic architecture: Examples from India
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2004.12.013openalex-snapshot
Microbially originated wrinkle structures on sandstone and their stratigraphic context: Palaeoproterozoic Koldaha Shale, central India
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2010.02.003openalex-snapshot
Interaction of microbial communities with clastic sedimentation during Palaeoproterozoic time — An example from basal Gulcheru Formation, Cuddapah basin, India
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2011.08.006openalex-snapshot
A case study of microbial mat-related features in coastal epeiric sandstones from the Paleoproterozoic Pretoria Group (Transvaal Supergroup, Kaapvaal craton, South Africa); The effect of preservation (reflecting sequence stratigraphic models) on the relationship between mat features and inferred…
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2015.04.007openalex-snapshot
Enigmatic carbonates of the Ombombo Subgroup, Otavi Fold Belt, Namibia: A prelude to extreme Cryogenian anoxia?
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2015.08.003openalex-snapshot
Paleoproterozoic microbially induced sedimentary structures from lagoonal depositional settings in northern China
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2016.11.002openalex-snapshot
Desiccation cracks in siliciclastic deposits: Microbial mat-related compared to abiotic sedimentary origin
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2020.105769openalex-snapshot
Manchuriophycus-like elliptical cracks in thin mudstones intercalated with lacustrine sandstone: Intrastratal crack formation in water-saturated sediments
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2026.107150openalex-snapshot
Types and formation mechanisms of diagenetic fractures in shale
inferred← citeshttps://doi.org/10.1016/s0012-8252(02)00158-7openalex-snapshot
Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal depositional systems (siliciclastic, evaporitic salty, and evaporitic carbonatic)
inferred← citeshttps://doi.org/10.1016/s0031-0182(03)00500-5openalex-snapshot
Bioturbation by symbiont-bearing annelids in near-anoxic sediments: Implications for biofacies models and paleo-oxygen assessments
inferred← citeshttps://doi.org/10.1016/s0037-0738(00)00098-1openalex-snapshot
Extensive microbial mats and their influences on the erosional and depositional dynamics of a siliciclastic cold water environment (Lower Arenigian, Montagne Noire, France)
inferred← citeshttps://doi.org/10.1016/s0037-0738(01)00083-5openalex-snapshot
Oceanography, bathymetry and syndepositional tectonics of a Precambrian intracratonic basin: integrating sediments, storms, earthquakes and tsunamis in the Belt Supergroup (Helena Formation, ca. 1.45Ga), western North America
inferred← citeshttps://doi.org/10.1016/s0037-0738(02)00103-3openalex-snapshot
Mat-related sedimentary structures in Neoproterozoic peritidal passive margin deposits of the West African Craton (Anti-Atlas, Morocco)
inferred← citeshttps://doi.org/10.1016/s0166-2635(04)80009-4openalex-snapshot
Sedimentation through time
inferred← citeshttps://doi.org/10.1016/s0166-2635(04)80011-2openalex-snapshot
Towards a Synthesis
inferred← citeshttps://doi.org/10.1016/s0166-2635(04)80016-1openalex-snapshot
References
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Implications of the Precambrian Non-stromatolitic Carbonate Succession Making up the Third Member of Mesoproterozoic Gaoyuzhuang Formation in Yanshan Area of North China
inferred← citeshttps://doi.org/10.1016/s1002-0705(08)60060-6openalex-snapshot
Microbial Mats in the Mesoproterozoic Carbonates of the North China Platform and Their Potential for Hydrocarbon Generation
inferred← citeshttps://doi.org/10.1016/s1872-5791(07)60017-7openalex-snapshot
Microbial Sand Chips in Transgressive Sandstones of the Precambrian: An Example from the Late Paleoproterozoic Dahongyu Formation at the Huyu Section of Nankou Town, Beijing, China
inferred← citeshttps://doi.org/10.1016/s1872-5791(07)60044-xopenalex-snapshot
Revised Classification of Microbial Carbonates: Complementing the Classification of Limestones
inferred← citeshttps://doi.org/10.1016/s1872-5791(08)60108-6openalex-snapshot
MISS in Mesoproterozoic Nonstromatolitic Limestones: A Case Study of the Third Member of Gaoyuzhuang Formation at Qiangou Section in Beijing
inferred← citeshttps://doi.org/10.1016/s1875-306x(07)80010-4openalex-snapshot
8 Ecosystem engineering in the fossil record: Early examples from the Cambrian Period
inferred← citeshttps://doi.org/10.1017/s0016756805000555openalex-snapshot
Fossils and matgrounds from the Neoproterozoic Longmyndian Supergroup, Shropshire, UK
inferred← citeshttps://doi.org/10.1017/s0016756812000507openalex-snapshot
Enigmatic sedimentary structures in the Lower Old Red Sandstone, south Wales, UK: possible microbial influence on surface processes and early terrestrial food webs
inferred← citeshttps://doi.org/10.1017/s0016756820001430openalex-snapshot
New insights into the early evolution of horizontal spiral trace fossils and the age of the Brioverian series (Ediacaran–Cambrian) in Brittany, NW France
inferred← citeshttps://doi.org/10.1017/s0016756822000097openalex-snapshot
Ordovician matground and mixground ecosystems in shoreface–offshore and barrier-island environments from Central Iran, northern Gondwana
inferred← citeshttps://doi.org/10.1017/s0016756824000086openalex-snapshot
Late Silurian event stratigraphy and facies of South Wales and the Welsh Borderland, United Kingdom
inferred← citeshttps://doi.org/10.1023/a:1004882619132openalex-snapshot
Microbial Mats As a Source of Carbonate Sediments in the Late Precambrian: Evidence from the Linok Formation, the Middle Riphean of the Turukhansk Uplift, Siberia
inferred← citeshttps://doi.org/10.1023/a:1020917505909openalex-snapshot
Microbial Mats and Terrigenous Sedimentation Settings in the Precambrian: The Middle Riphean Bezymyannyi Formation of the Turukhansk Uplift
inferred← citeshttps://doi.org/10.1038/ncomms4544openalex-snapshot
Ediacaran matground ecology persisted into the earliest Cambrian
inferred← citeshttps://doi.org/10.1038/ngeo1142openalex-snapshot
Possible evolution of mobile animals in association with microbial mats
inferred← citeshttps://doi.org/10.1046/j.1365-3091.2000.00003.xopenalex-snapshot
Microbial carbonates: the geological record of calcified bacterial–algal mats and biofilms
inferred← citeshttps://doi.org/10.1080/10420940.2016.1216845openalex-snapshot
Arthropod Trace Fossils of the Upper Lower Cambrian Gog Group, Southern Rocky Mountains of Canada
inferred← citeshttps://doi.org/10.1080/10420940.2017.1294590openalex-snapshot
An Ichnotaxonomic Approach to Wrinkled Microbially Induced Sedimentary Structures
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Stratigraphic and Paleobiogeographic Distribution ofArthrophycus
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Defining the IchnogenusArthrophycusUsing Numerical Taxonomic Methods
inferred← citeshttps://doi.org/10.1080/10420940.2021.1932494openalex-snapshot
Oldhamiafrom the Oligocene/Miocene-age deep-marine Algeciras Unit, Campo de Gibraltar Complex, southeast Spain: First record of this characteristic Lower Palaeozoic (mainly Cambrian) ichnofossil from younger strata
inferred← citeshttps://doi.org/10.1080/10420940109380180openalex-snapshot
Are meandering structures found in proterozoic rocks of different ages of the Vindhyan supergroup of central India biogenic?: A scrutiny
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Spirodesmos milanain. isp.: A Shallow-Water Spiral Trace Fossil from the Cambrian of the Eastern Cordillera, Northwest Argentina
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A New Ichnospecies ofArthrophycusfrom the Upper Cambrian-Lower Tremadocian of Northwest Argentina: Implications for the Arthrophycid Lineage and Potential in Ichnostratigraphy
inferred← citeshttps://doi.org/10.1089/ast.2008.0290openalex-snapshot
Development of Lower Triassic Wrinkle Structures: Implications for the Search for Life on Other Planets
inferred← citeshttps://doi.org/10.1098/rsta.2012.0362openalex-snapshot
Formation of Kinneyia via shear-induced instabilities in microbial mats
inferred← citeshttps://doi.org/10.1109/tgrs.2024.3367632openalex-snapshot
Searching for Life: End-to-End Automated Detection and Characterization of Ediacaran Biosignatures
inferred← citeshttps://doi.org/10.1111/gbi.12038openalex-snapshot
Global deglaciation and the re‐appearance of microbial matground‐dominated ecosystems in the late P aleozoic of G ondwana
inferred← citeshttps://doi.org/10.1111/gbi.12296openalex-snapshot
Unusual microbial mat‐related structural diversity 2.1 billion years ago and implications for the Francevillian biota
inferred← citeshttps://doi.org/10.1111/gbi.12473openalex-snapshot
The interplay of environmental constraints and bioturbation on matground development along the marine depositional profile during the Ordovician Radiation
inferred← citeshttps://doi.org/10.1111/gbi.12580openalex-snapshot
Microbial mats and their palaeoenvironmental analysis in offshore – shelf facies of the Los Molles Formation (Toarcian – Lower Callovian) in the Chacay Melehue area, Neuquén Basin, Argentina
inferred← citeshttps://doi.org/10.1111/j.0031-0239.2000.00134.xopenalex-snapshot
The first named Ediacaran body fossil, Aspidella Terranovica
inferred← citeshttps://doi.org/10.1111/j.1365-3091.2010.01215.xopenalex-snapshot
Alluvial facies evolution during the Palaeozoic greening of the continents: case studies, conceptual models and modern analogues
inferred← citeshttps://doi.org/10.1111/j.1468-8123.2007.00189.xopenalex-snapshot
Seabed Fluid Flow
inferred← citeshttps://doi.org/10.1111/j.1472-4669.2007.00128.xopenalex-snapshot
Calcium carbonate precipitation in cyanobacterial mats from sandy tidal flats of the North Sea
inferred← citeshttps://doi.org/10.1111/j.1755-6724.2008.tb00580.xopenalex-snapshot
Sedimentary Features and Implications for the Precambrian Non‐stromatolitic Carbonate Succession: A Case Study of the Mesoproterozoic Gaoyuzhuang Formation at the Qiangou Section in Yanqing County of Beijing
inferred← citeshttps://doi.org/10.1111/j.1755-6724.2011.00242.xopenalex-snapshot
Molar Tooth Structure: a Contribution from the Mesoproterozoic Gaoyuzhuang Formation, Tianjin City, North China
inferred← citeshttps://doi.org/10.1111/let.12280openalex-snapshot
Microbially induced wrinkle structures in Middle Devonian siliciclastics from the Prague Basin, Czech Republic
inferred← citeshttps://doi.org/10.1111/sed.12044openalex-snapshot
Microbial mats implicated in the generation of intrastratal shrinkage (‘synaeresis’) cracks
inferred← citeshttps://doi.org/10.1111/sed.12745openalex-snapshot
Palaeoecological, sedimentological and stratigraphical insights into microbially induced sedimentary structures of the lower Cambrian successions of Iran
inferred← citeshttps://doi.org/10.1130/0091-7613(2001)029<0763:cocfga>2.0.co;2openalex-snapshot
Calcification of cyanobacterial filaments: Girvanella and the origin of lower Paleozoic lime mud
inferred← citeshttps://doi.org/10.1130/0091-7613(2002)030<0343:cposge>2.0.co;2openalex-snapshot
Clingfilm preservation of spiraliform graptolites: Evidence of organically sealed Silurian seafloors
inferred← citeshttps://doi.org/10.1130/0091-7613(2002)030<0811:lolitp>2.0.co;2openalex-snapshot
Life on land in the Proterozoic: Evidence from the Torridonian rocks of northwest Scotland
inferred← citeshttps://doi.org/10.1130/b35229.1openalex-snapshot
Controls on the formation of microbially induced sedimentary structures and biotic recovery in the Lower Triassic of Arctic Canada
inferred← citeshttps://doi.org/10.1130/g21185.1openalex-snapshot
A Late Silurian extinction event and anachronistic period
inferred← citeshttps://doi.org/10.1130/g22722a.1openalex-snapshot
Spiral-shaped graphoglyptids from an Early Permian intertidal flat
inferred← citeshttps://doi.org/10.1130/g37791.1openalex-snapshot
Insights into cyanobacterial fossilization in Ediacaran siliciclastic environments
inferred← citeshttps://doi.org/10.1130/gsatg7a.1openalex-snapshot
Turbulent lifestyle: Microbial mats on Earth's sandy beaches—Today and 3 billion years ago
inferred← citeshttps://doi.org/10.1134/s0024490211020076openalex-snapshot
Facies characteristics and terrigenous sedimentation features of the lower Riphean Mukun Group (Anabar Uplift, Siberia)
inferred← citeshttps://doi.org/10.1134/s0024490214010039openalex-snapshot
The Mukun basin: Settings, paleoenvironmental parameters, and factors controlling the early mesoproterozoic terrestrial sedimentation (Lower Riphean section of the Anabar uplift, Siberia)
inferred← citeshttps://doi.org/10.1134/s0031030115040139openalex-snapshot
Microbial factor in the formation of sedimentary continental systems of the Proterozoic (Mukun Basin, Lower Riphean of the Anabar Uplift of Siberia)
inferred← citeshttps://doi.org/10.1144/sp286.1openalex-snapshot
Insights in the Neoproterozoic–Early Cambrian transition of NW Argentina: facies, environments and fossils in the proto-margin of western Gondwana
inferred← citeshttps://doi.org/10.1144/sp448.15openalex-snapshot
The origin and occurrence of subaqueous sedimentary cracks
inferred← citeshttps://doi.org/10.1144/sp522-2020-269openalex-snapshot
Exotic facies episodes of a carbonate platform: implications for middle and late Cambrian ecosystems and impact of bioturbation in the Alborz Basin, Iran
inferred← citeshttps://doi.org/10.1144/sp556-2024-133openalex-snapshot
Distinguishing microbially induced sedimentary structures from flow-induced interfacial deformation structures (MISS v. FIDS)
inferred← citeshttps://doi.org/10.1306/010302720589openalex-snapshot
Microbially Induced Sedimentary Structures—A New Category Within the Classification of Primary Sedimentary Structures—Reply
inferred← citeshttps://doi.org/10.1306/040404740914openalex-snapshot
Origin of Meter-Scale Submarine Cavities and Herringbone Calcite Cement in a Cambrian Microbial Reef, Ledger Formation (U.S.A.)
inferred← citeshttps://doi.org/10.1306/2dc4095d-0e47-11d7-8643000102c1865dopenalex-snapshot
Microbially Induced Sedimentary Structures: A New Category within the Classification of Primary Sedimentary Structures
inferred← citeshttps://doi.org/10.1515/geoca-2017-0030openalex-snapshot
Asteriacites and other trace fossils from the Po Formation (Visean–Serpukhovian), Ganmachidam Hill, Spiti Valley (Himalaya) and its paleoenvironmental significance
inferred← citeshttps://doi.org/10.1666/13-054openalex-snapshot
Scratch Traces of Large Ediacara Bilaterian Animals
inferred← citeshttps://doi.org/10.1669/0883-1351(2002)017<0533:scotfa>2.0.co;2openalex-snapshot
Sedimentary Controls on the Formation and Preservation of Microbial Mats in Siliciclastic Deposits: A Case Study from the Upper Neoproterozoic Nama Group, Namibia
inferred← citeshttps://doi.org/10.1669/0883-1351(2003)018<0572:ecotds>2.0.co;2openalex-snapshot
Early Colonization of the Deep Sea: Ichnologic Evidence of Deep-marine Benthic Ecology from the Early Cambrian of Northwest Argentina
inferred← citeshttps://doi.org/10.18261/9788294167128-2025-01openalex-snapshot
Ichnology of the Ediacaran–Cambrian Chapel Island Formation of Newfoundland, Canada: unraveling bioturbation at the onset of the Cambrian Explosion
inferred← citeshttps://doi.org/10.18814/epiiugs/2012/v35i4/008openalex-snapshot
Microbial mat related structures (MRS) from Mesoproterozoic Chhattisgarh and Khariar basins, Central India and their bearing on shallow marine sedimentation
inferred← citeshttps://doi.org/10.2110/jsr.2020.17openalex-snapshot
Paleoenvironmental significance of microbial mat-related structures and ichnofaunas in an Ordovician mixed-energy estuary, Áspero Formation of Santa Victoria Group, northwestern Argentina
inferred← citeshttps://doi.org/10.2110/jsr.2023.111openalex-snapshot
Microbially induced sedimentary structures (MISS s ) in Early Devonian siliciclastic deposits (Gara Djebilet Formation, Tindouf Basin, Algerian Sahara)
inferred← citeshttps://doi.org/10.2110/palo.2003.p03-08openalex-snapshot
Trace Fossils and Paleoenvironments of a Late Silurian Marginal-Marine/Alluvial System: the Ringerike Group (Lower Old Red Sandstone), Oslo Region, Norway
inferred← citeshttps://doi.org/10.2110/palo.2006.p06-095ropenalex-snapshot
Kinneyia-Type Wrinkle Structures—Critical Review And Model Of Formation
inferred← citeshttps://doi.org/10.2110/palo.2006.p06-104ropenalex-snapshot
STRANDED IN UPSTATE NEW YORK: CAMBRIAN SCYPHOMEDUSAE FROM THE POTSDAM SANDSTONE
inferred← citeshttps://doi.org/10.2110/palo.2009.p09-079ropenalex-snapshot
EARLY MOLLUSCAN EVOLUTION: EVIDENCE FROM THE TRACE FOSSIL RECORD
inferred← citeshttps://doi.org/10.2110/palo.2012.p12-122ropenalex-snapshot
CARBONATE RETICULATED RIDGE STRUCTURES FROM THE LOWER MIDDLE TRIASSIC OF THE LUOPING AREA, YUNNAN, SOUTHWESTERN CHINA: GEOBIOLOGIC FEATURES AND IMPLICATIONS FOR EXCEPTIONAL PRESERVATION OF THE LUOPING BIOTA
inferred← citeshttps://doi.org/10.2110/palo.2013.073openalex-snapshot
MICROBIAL MATS AND ICHNOFAUNA OF A FLUVIAL-TIDAL CHANNEL IN THE LOWER PENNSYLVANIAN JOGGINS FORMATION, CANADA
inferred← citeshttps://doi.org/10.2110/palo.2016.028openalex-snapshot
INVERTED TRILOBITES: KEY TO COMPLEX PRESERVATION OF AN ORGANICALLY TEXTURED SURFACE IN OFFSHORE SILICICLASTIC MUDSTONE AND CARBONATE FACIES: KOPE FORMATION (UPPER ORDOVICIAN), KENTON COUNTY, KENTUCKY, USA
inferred← citeshttps://doi.org/10.2110/palo.2016.064openalex-snapshot
SHORT-TERM EVOLUTION OF PRIMARY SEDIMENTARY SURFACE TEXTURES (MICROBIAL, ABIOTIC, ICHNOLOGICAL) ON A DRY STREAM BED: MODERN OBSERVATIONS AND ANCIENT IMPLICATIONS
inferred← citeshttps://doi.org/10.2110/palo.2021.015openalex-snapshot
KINNEYIA-TYPE WRINKLE STRUCTURES ON SANDSTONE BEDS: NOT MICROBIALLY INDUCED BUT DEFORMATION FEATURES CAUSED BY SYNSEDIMENTARY EARTHQUAKES
inferred← citeshttps://doi.org/10.2110/palo.2023.018openalex-snapshot
THE MICROBIAL “FINGERPRINTS” FROM THE CONTINENTAL LOWER PERMIAN OF POLAND
inferred← citeshttps://doi.org/10.2110/palo.2025.042openalex-snapshot
MICROBIAL MAT FACIES IN CAMBRIAN TIDAL FLATS AND IMPLICATIONS FOR THE TRACE FOSSIL RECORD (ELK MOUND GROUP, WISCONSIN, USA)
inferred← citeshttps://doi.org/10.2110/sepmsp.101.015openalex-snapshot
The Trace-Fossil Record of Organism–matground Interactions in Space and Time
inferred← citeshttps://doi.org/10.2110/sepmsp.101.029openalex-snapshot
The Record of Microbially Induced Sedimentary Structures (MISS) in the Swedish Paleozoic
inferred← citeshttps://doi.org/10.2110/sepmsp.101.139openalex-snapshot
Criteria for Distinguishing Microbial Mats and Earths
inferred← citeshttps://doi.org/10.2110/sepmsp.101.163openalex-snapshot
Morphological Association of Microbially Induced Sedimentary Structures (MISS) as a Paleoenvironmental Indicator
inferred← citeshttps://doi.org/10.2517/2015pr009openalex-snapshot
Macroorganism Paleoecosystems During the Middle-Late Ediacaran Period in the Yangtze Block, South China
inferred← citeshttps://doi.org/10.31084/2619-0087/2025-3-6openalex-snapshot
Lithological indicators of storm sedimentation in the deposits of the BederyshSubformation of the Upper Riphean Zilmerdak Formation, Southern Urals
inferred← citeshttps://doi.org/10.3319/tao.2005.16.5.1097(t)openalex-snapshot
Characteristic Trace Fossils from Shoreface to Offshore Environments of an Oligocene Succession, Northeastern Taiwan
inferred← citeshttps://doi.org/10.3389/fmats.2016.00030openalex-snapshot
Kinneyia: A Flow-Induced Anisotropic Fossil Pattern from Ancient Microbial Mats
inferred← citeshttps://doi.org/10.3390/life12020136openalex-snapshot
Were the First Trace Fossils Really Burrows or Could They Have Been Made by Sediment-Displacive Chemosymbiotic Organisms?
inferred← citeshttps://doi.org/10.3724/sp.j.1261.2014.00048openalex-snapshot
Palaeoenvironmental and biostratigraphic implications of microbial mat-related structures: Examples from the modern Gulf of Cambay and the Precambrian Vindhyan Basin, India
inferred← citeshttps://doi.org/10.4138/atlgeol.2011.003openalex-snapshot
Insights into an Early Jurassic dinosaur habitat: ichnofacies and enigmatic structures from the Portland Formation, Hoover Quarry, Massachusetts, U.S.A.
inferred← citeshttps://doi.org/10.57035/journals/sdk.2023.e11.1083openalex-snapshot
Tectonic, eustatic and climate controls on facies architecture during the transition to the Neoproterozoic icehouse in the Adelaide Superbasin, Australia
inferred← citeshttps://doi.org/10.70675/5aab44dcz6310z42beza3d0zc3672a46b0c5openalex-snapshot
Étude multi-approches des voiles bactériens du Paléoprotérozoïque (2,1 Ga, Gabon) : Biogénicité, minéralogie et biogéochimie
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