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When Life Got Smart: The Evolution of Behavioral Complexity Through the Ediacaran and Early Cambrian of NW Canada
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Outgoing claims: the papers this work cites, builds on, or argues with.
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Neoproterozoic Geobiology and Paleobiology
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Textured organic surfaces associated with the Ediacara biota in South Australia
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Trace fossil evidence for Ediacaran bilaterian animals with complex behaviors
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Chapter 11 Evolution of Trace Fossil Communities
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A placozoan affinity for Dickinsonia and the evolution of late Proterozoic metazoan feeding modes
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Fossil Foraging Behavior: Computer Simulation
inferredcites →https://doi.org/10.1126/science.221.4609.455openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.270.5236.598openalex-snapshot
Biostratigraphic and Geochronologic Constraints on Early Animal Evolution
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Late Jurassic selachians (Chondrichthyes: Hybodontiformes, Neoselachii) from Central Portugal
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Integrated chemostratigraphy and biostratigraphy of the Windermere Supergroup, northwestern Canada: Implications for Neoproterozoic correlations and the early evolution of animals
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inferredcites →https://doi.org/10.1130/0091-7613(2003)031<0431:eocana>2.0.co;2openalex-snapshot
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inferredcites →https://doi.org/10.1130/g30368.1openalex-snapshot
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Ediacaran body and trace fossils in Miette Group (Windermere Supergroup) near Salient Mountain, British Columbia, CanadaRevision of the paper was carried out by Dr. Guy Narbonne following the passing away of both Hans Hofmann (†deceased May 19, 2010) and Eric Mountjoy (†deceased June 18, 2010)…
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inferredcites →https://doi.org/10.18261/8200376656-1997-01openalex-snapshot
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Ediacaran biota of the Wernecke Mountains, Yukon, Canada
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inferred← citeshttps://doi.org/10.1016/j.annpal.2022.102543openalex-snapshot
Quantitative analysis of horizontal bioturbation from Brioverian (Ediacaran - Fortunian) deposits of Brittany (Armorican Massif, NW of France)
inferred← citeshttps://doi.org/10.1016/j.annpal.2023.102629openalex-snapshot
Biotic vs abiotic origin of unusual features from Mesoproterozoic of Vindhyan Supergroup, India
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2016.12.010openalex-snapshot
Was the Ediacaran Shuram Excursion a globally synchronized early diagenetic event? Insights from methane-derived authigenic carbonates in the uppermost Doushantuo Formation, South China
inferred← citeshttps://doi.org/10.1016/j.cub.2015.09.066openalex-snapshot
Uncertainty in the Timing of Origin of Animals and the Limits of Precision in Molecular Timescales
inferred← citeshttps://doi.org/10.1016/j.cub.2016.09.012openalex-snapshot
Fossils and the Evolution of the Arthropod Brain
inferred← citeshttps://doi.org/10.1016/j.cub.2024.11.028openalex-snapshot
Environmental and evolutionary controls in animal-sediment interactions at the onset of the Cambrian explosion
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.2017.08.009openalex-snapshot
The Cambrian revolutions: Trace-fossil record, timing, links and geobiological impact
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.01.011openalex-snapshot
The early Paleozoic development of bioturbation—Evolutionary and geobiological consequences
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103435openalex-snapshot
The trace fossil record of the Nama Group, Namibia: Exploring the terminal Ediacaran roots of the Cambrian explosion
inferred← citeshttps://doi.org/10.1016/j.earscirev.2022.103971openalex-snapshot
The Psammichnites-Taphrhelminthopsis conundrum: Implications for Calibrating the Cambrian explosion
inferred← citeshttps://doi.org/10.1016/j.earscirev.2022.104017openalex-snapshot
Locating the BACE of the Cambrian: Bayan Gol in southwestern Mongolia and global correlation of the Ediacaran–Cambrian boundary
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.105009openalex-snapshot
Terminal Ediacaran–Terreneuvian revolutions in Siberia
inferred← citeshttps://doi.org/10.1016/j.gca.2024.04.018openalex-snapshot
Trends in estuarine pyrite formation point to an alternative model for Paleozoic pyrite burial
inferred← citeshttps://doi.org/10.1016/j.gr.2014.11.002openalex-snapshot
Remarkable insights into the paleoecology of the Avalonian Ediacaran macrobiota
inferred← citeshttps://doi.org/10.1016/j.isci.2021.102271openalex-snapshot
Deciphering trophic interactions in a mid-Cambrian assemblage
inferred← citeshttps://doi.org/10.1016/j.isci.2022.105916openalex-snapshot
Ants combine systematic meandering and correlated random walks when searching for unknown resources
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.palaeo.2017.03.012openalex-snapshot
Discriminating ecological and evolutionary controls during the Ediacaran–Cambrian transition: Trace fossils from the Soltanieh Formation of northern Iran
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109333openalex-snapshot
The trace fossil Thalassinoides bacae in the Cambrian Zhangxia Formation (Miaolingian Series) of North China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110255openalex-snapshot
Deep-time geometricians and hints on motor control evolution of marine invertebrates
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110672openalex-snapshot
The conquest of spaces: Exploring drivers of morphological shifts through phylogenetic palaeoecology
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112126openalex-snapshot
The Lower Cambrian deposits of the Le Rozel Formation (Normandy, NW France): Insight into a newly described ichnofossil assemblage
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113607openalex-snapshot
Reestablishment of an early life shallow marine ecosystem in the Neoproterozoic Gardnos meteorite impact crater (Norway)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114045openalex-snapshot
Three-dimensional burrow systems reveal high behavioral complexity and intense bioturbation at the Ediacaran-Cambrian transition
inferred← citeshttps://doi.org/10.1016/j.palwor.2021.01.002openalex-snapshot
Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
inferred← citeshttps://doi.org/10.1016/j.precamres.2017.08.012openalex-snapshot
The ins and outs of Ediacaran discs
inferred← citeshttps://doi.org/10.1016/j.precamres.2019.105507openalex-snapshot
Cryogenian Aspidella from northwestern Canada
inferred← citeshttps://doi.org/10.1016/j.precamres.2020.105627openalex-snapshot
Complex tunnel systems of early Fortunian macroscopic endobenthos in the Ediacaran-Cambrian transitional strata of the Olenek Uplift (NE Siberian Platform)
inferred← citeshttps://doi.org/10.1016/j.precamres.2020.105721openalex-snapshot
The Ediacaran–Cambrian boundary: Evaluating stratigraphic completeness and the Great Unconformity
inferred← citeshttps://doi.org/10.1016/j.precamres.2022.106710openalex-snapshot
Sequence stratigraphy and paleoenvironmental significance of the Neoproterozoic Bambui Group, Central Brazil
inferred← citeshttps://doi.org/10.1016/j.precamres.2023.107227openalex-snapshot
First record of trace fossils in the Ediacaran–Cambrian transition on the northern Gondwana platform (Anti-Atlas, Morocco)
inferred← citeshttps://doi.org/10.1016/j.precamres.2023.107238openalex-snapshot
Shadows of the past: An Ediacara-style taphonomic window in advent of Cambrian bioturbators
inferred← citeshttps://doi.org/10.1016/j.precamres.2024.107307openalex-snapshot
Ediacaran tectographs from the Itajaí Basin: A cautionary tale from the Precambrian
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/10.1017/jpa.2014.25openalex-snapshot
New Ediacaran fossils from the uppermost Blueflower Formation, northwest Canada: disentangling biostratigraphy and paleoecology
inferred← citeshttps://doi.org/10.1017/jpa.2016.20openalex-snapshot
A new reconstruction of continentalTreptichnusbased on exceptionally preserved material from the Jurassic of Massachusetts
inferred← citeshttps://doi.org/10.1017/jpa.2017.72openalex-snapshot
Ichnostratigraphy of the Ediacaran-Cambrian boundary: new insights on lower Cambrian biozonations from the Soltanieh Formation of northern Iran
inferred← citeshttps://doi.org/10.1017/jpa.2017.92openalex-snapshot
RETRACTED—Eldonioids with associated trace fossils from the lower Cambrian Emu Bay Shale Konservat-Lagerstätte of South Australia
inferred← citeshttps://doi.org/10.1017/jpa.2018.6openalex-snapshot
Eldonioids with associated trace fossils from the lower Cambrian Emu Bay Shale Konservat-Lagerstätte of South Australia
inferred← citeshttps://doi.org/10.1017/pab.2016.20openalex-snapshot
Ediacaran distributions in space and time: testing assemblage concepts of earliest macroscopic body fossils
inferred← citeshttps://doi.org/10.1017/pab.2021.46openalex-snapshot
The Phanerozoic aftermath of the Cambrian information revolution: sensory and cognitive complexity in marine faunas
inferred← citeshttps://doi.org/10.1017/s0016756816001369openalex-snapshot
Lowermost Cambrian acritarchs from the Yanjiahe Formation, South China: implication for defining the base of the Cambrian in the Yangtze Platform
inferred← citeshttps://doi.org/10.1017/s0016756819000141openalex-snapshot
A protracted Ediacaran–Cambrian transition: an ichnologic ecospace analysis of the Fortunian in Newfoundland, Canada
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/s0016756821000327openalex-snapshot
Scratching the discs: evaluating alternative hypotheses for the origin of the Ediacaran discoidal structures from the Cerro Negro Formation, La Providencia Group, Argentina
inferred← citeshttps://doi.org/10.1017/s0016756821001187openalex-snapshot
Distribution and correlation ofSabellidites cambriensis(Annelida?) in the basal Cambrian on Baltica
inferred← citeshttps://doi.org/10.1017/s1089332600002904openalex-snapshot
Late Proterozoic–Early Phanerozoic ‘Taphonomic Windows’: The Environmental and Temporal Distribution of Recurrent Modes of Exceptional Preservation
inferred← citeshttps://doi.org/10.1038/s41467-023-39030-2openalex-snapshot
The monoaminergic system is a bilaterian innovation
inferred← citeshttps://doi.org/10.1038/s41559-017-0138openalex-snapshot
The energy expansions of evolution
inferred← citeshttps://doi.org/10.1038/s41559-019-0821-6openalex-snapshot
Integrated records of environmental change and evolution challenge the Cambrian Explosion
inferred← citeshttps://doi.org/10.1038/s41598-018-22859-9openalex-snapshot
Sediment disturbance by Ediacaran bulldozers and the roots of the Cambrian explosion
inferred← citeshttps://doi.org/10.1038/srep45539openalex-snapshot
Rheotaxis in the Ediacaran epibenthic organism Parvancorina from South Australia
inferred← citeshttps://doi.org/10.1073/pnas.1403669112openalex-snapshot
The advent of animals: The view from the Ediacaran
inferred← citeshttps://doi.org/10.1080/03115518.2016.1159412openalex-snapshot
Ediacaran fossils in thin-section
inferred← citeshttps://doi.org/10.1080/08120099.2025.2586733openalex-snapshot
New trail-like features associated with microbial mats from the early Neoproterozoic Sirbu Shale Member (Upper Vindhyan Group), Vindhyan Basin, central India
inferred← citeshttps://doi.org/10.1080/10420940.2015.1127232openalex-snapshot
New Occurrences ofOldhamiain Eastern Yukon, Canada: Stratigraphic Context and Implications for Cambrian Deep-Marine Biostratigraphy
inferred← citeshttps://doi.org/10.1080/10420940.2017.1308865openalex-snapshot
Trace Fossils from the Brioverian (Ediacaran–Fortunian) in Brittany (NW France)
inferred← citeshttps://doi.org/10.1080/10420940.2021.1932490openalex-snapshot
Ichnology and biostratigraphic significance of Cambrian trace fossils from the lowest stratigraphic level of Kunzam La Formation, Chandra Valley, Lahaul and Spiti, India
inferred← citeshttps://doi.org/10.1080/10420940.2021.1932491openalex-snapshot
Psammichnites gigasfrom the lower Cambrian of the Mackenzie Mountains, northwest Canada, and their biostratigraphic implications
inferred← citeshttps://doi.org/10.1080/10420940.2026.2642060openalex-snapshot
Reproducing and understanding a fossil trail in digitized worlds: a protocol to quantitative analyses of movement trajectories
inferred← citeshttps://doi.org/10.1080/14772019.2026.2681697openalex-snapshot
Trajectory smoothness – an important criterion in ichnotaxonomy and its implications for identifying tracemakers
inferred← citeshttps://doi.org/10.1086/706252openalex-snapshot
The Evolutionary Origin of Associative Learning
inferred← citeshttps://doi.org/10.1093/9780197797464.003.0005openalex-snapshot
Animals and Individuals
inferred← citeshttps://doi.org/10.1093/9780197797464.003.0009openalex-snapshot
The Early Cambrian Fossils
inferred← citeshttps://doi.org/10.1093/icb/icy020openalex-snapshot
Ecological Expansion and Extinction in the Late Ediacaran: Weighing the Evidence for Environmental and Biotic Drivers
inferred← citeshttps://doi.org/10.1098/rsfs.2019.0103openalex-snapshot
The rise and early evolution of animals: where do we stand from a trace-fossil perspective?
inferred← citeshttps://doi.org/10.1098/rsos.190548openalex-snapshot
Increase in metazoan ecosystem engineering prior to the Ediacaran–Cambrian boundary in the Nama Group, Namibia
inferred← citeshttps://doi.org/10.1098/rspb.2015.1003openalex-snapshot
Biotic replacement and mass extinction of the Ediacara biota
inferred← citeshttps://doi.org/10.1098/rspb.2021.0061openalex-snapshot
Symbiosis in the Cambrian: enteropneust tubes from the Burgess Shale co-inhabited by commensal polychaetes
inferred← citeshttps://doi.org/10.1098/rspb.2024.1629openalex-snapshot
Identifying signatures of the earliest benthic bulldozers in emergent subaerial conditions during the colonization of land by animals
inferred← citeshttps://doi.org/10.1098/rspb.2025.0889openalex-snapshot
Smoothness analyses of trace fossils: expanding quantitative toolkits to unravel bilaterian movement ecology during the Ediacaran–Cambrian transition
inferred← citeshttps://doi.org/10.1098/rstb.2015.0034openalex-snapshot
Introduction to ‘Homology and convergence in nervous system evolution’
inferred← citeshttps://doi.org/10.1098/rstb.2015.0037openalex-snapshot
Early animal evolution and the origins of nervous systems
inferred← citeshttps://doi.org/10.1101/219444openalex-snapshot
Cross-species systems analysis of evolutionary toolkits of neurogenomic response to social challenge
inferred← citeshttps://doi.org/10.1111/brv.13014openalex-snapshot
Decline and fall of the Ediacarans: late‐Neoproterozoic extinctions and the rise of the modern biosphere
inferred← citeshttps://doi.org/10.1111/gbb.12502openalex-snapshot
Cross‐species systems analysis of evolutionary toolkits of neurogenomic response to social challenge
inferred← citeshttps://doi.org/10.1111/gbi.12178openalex-snapshot
Environmental context for the terminal Ediacaran biomineralization of animals
inferred← citeshttps://doi.org/10.1111/gbi.12597openalex-snapshot
Deep‐water first occurrences of Ediacara biota prior to the Shuram carbon isotope excursion in the Wernecke Mountains, Yukon, Canada
inferred← citeshttps://doi.org/10.1111/pala.12732openalex-snapshot
Bioturbators as ecosystem engineers in space and time
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/10.1111/sed.70094openalex-snapshot
The relationship between organic matgrounds and sedimentary packaging: examples from the Ediacaran and early Cambrian
inferred← citeshttps://doi.org/10.1126/sciadv.adk2152openalex-snapshot
Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era
inferred← citeshttps://doi.org/10.1126/sciadv.adu7719openalex-snapshot
Tracking bioturbation through time: The evolution of the marine sedimentary mixed and transition layers
inferred← citeshttps://doi.org/10.1126/sciadv.adx9449openalex-snapshot
Advent of three-dimensional sediment exploration reveals Ediacaran-Cambrian ecosystem transition
inferred← citeshttps://doi.org/10.1126/sciadv.aed9916openalex-snapshot
Discovery of White Sea assemblage fossils from Laurentia
inferred← citeshttps://doi.org/10.1130/b31329.1openalex-snapshot
Oxygen, facies, and secular controls on the appearance of Cryogenian and Ediacaran body and trace fossils in the Mackenzie Mountains of northwestern Canada
inferred← citeshttps://doi.org/10.1130/g47234.1openalex-snapshot
Microbially induced pseudotraces from a Pantanal soda lake, Brazil: Alternative interpretations for Ediacaran simple trails and their limits
inferred← citeshttps://doi.org/10.1130/g53332.1openalex-snapshot
Quantitative decoding of Ediacaran locomotory trace fossil morphologies: Evidence for the emergence of slender anterior-posterior body profiles
inferred← citeshttps://doi.org/10.1130/geol.s.12298484openalex-snapshot
Supplemental Material: Microbially induced pseudotraces from a Pantanal soda lake, Brazil: Alternative interpretations for Ediacaran simple trails and their limits
inferred← citeshttps://doi.org/10.1130/geol.s.12298484.v1openalex-snapshot
Supplemental Material: Microbially induced pseudotraces from a Pantanal soda lake, Brazil: Alternative interpretations for Ediacaran simple trails and their limits
inferred← citeshttps://doi.org/10.1130/gsatg265a.1openalex-snapshot
The Latest Ediacaran Wormworld Fauna: Setting the Ecological Stage for the Cambrian Explosion
inferred← citeshttps://doi.org/10.1139/cjes-2017-0274openalex-snapshot
Effects of bioturbation on carbon and sulfur cycling across the Ediacaran–Cambrian transition at the GSSP in Newfoundland, Canada
inferred← citeshttps://doi.org/10.1144/sp448.18openalex-snapshot
Engineering the Cambrian explosion: the earliest bioturbators as ecosystem engineers
inferred← citeshttps://doi.org/10.1144/sp448.9openalex-snapshot
Martin Brasier's contribution to the palaeobiology of the Ediacaran–Cambrian transition
inferred← citeshttps://doi.org/10.11606/t.44.2022.tde-10022023-091906openalex-snapshot
Icnofósseis das Formações Tamengo e Guaicurus, Grupo Corumbá: implicações paleoambientais e paleoecológicasGICAS
inferred← citeshttps://doi.org/10.1666/13-000iopenalex-snapshot
An Examination of Life History and Behavioral Evolution Across the Ediacaran–Cambrian Transition
inferred← citeshttps://doi.org/10.1666/13-042openalex-snapshot
Trace Fossils with Spreiten from the Late Ediacaran Nama Group, Namibia: Complex Feeding Patterns Five Million Years Before the Precambrian–Cambrian Boundary
inferred← citeshttps://doi.org/10.1666/13-053openalex-snapshot
Deep-Water Ediacaran Fossils from Northwestern Canada: Taphonomy, Ecology, and Evolution
inferred← citeshttps://doi.org/10.1666/13-056openalex-snapshot
Diachronous Increase in Early Cambrian Ichnofossil Size and Benthic Faunal Activity in Different Climatic Regions
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/10.18261/let.57.3.8openalex-snapshot
The largest complex burrow system from the early Cambrian of Sweden, probably made by priapulids in response to tidal currents
inferred← citeshttps://doi.org/10.18814/epiiugs/2014/v37i3/007openalex-snapshot
International Symposium and Field Workshop on Ediacaran and Cryogenian Stratigraphy
inferred← citeshttps://doi.org/10.18814/epiiugs/2016/v39i4/103886openalex-snapshot
Towards an Ediacaran Time Scale: Problems, Protocols, and Prospects
inferred← citeshttps://doi.org/10.2110/jsr.2016.19openalex-snapshot
Microbial Origin of Early Animal Trace Fossils?
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/palo.2014.011openalex-snapshot
CONFIRMING THE METAZOAN CHARACTER OF A 565 MA TRACE-FOSSIL ASSEMBLAGE FROM MISTAKEN POINT, NEWFOUNDLAND
inferred← citeshttps://doi.org/10.2110/palo.2015.095openalex-snapshot
FRAMBOIDAL PYRITE SHROUD CONFIRMS THE ‘DEATH MASK' MODEL FOR MOLDIC PRESERVATION OF EDIACARAN SOFT-BODIED ORGANISMS
inferred← citeshttps://doi.org/10.2110/palo.2016.060openalex-snapshot
MICROBIAL MAT SANDWICHES AND OTHER ANACTUALISTIC SEDIMENTARY FEATURES OF THE EDIACARA MEMBER (RAWNSLEY QUARTZITE, SOUTH AUSTRALIA): IMPLICATIONS FOR INTERPRETATION OF THE EDIACARAN SEDIMENTARY RECORD
inferred← citeshttps://doi.org/10.2110/palo.2021.050openalex-snapshot
THE ROLE OF SURFICIAL BIOTURBATION IN THE LATEST EDIACARAN: A QUANTITATIVE ANALYSIS OF TRACE FOSSIL INTENSITY IN THE TERMINAL EDIACARAN–LOWER CAMBRIAN OF CALIFORNIA
inferred← citeshttps://doi.org/10.2110/palo.2025.049openalex-snapshot
EARLIEST EVIDENCE FOR OVERGROWTH AMONG EDIACARAN FRONDS AT NILPENA EDIACARA NATIONAL PARK, SOUTH AUSTRALIA
inferred← citeshttps://doi.org/10.2113/rgg20234595openalex-snapshot
Preservation of Soft-Bodied Organisms in Early Cambrian Carbonates
inferred← citeshttps://doi.org/10.2139/ssrn.6123652openalex-snapshot
Three-dimensional burrow systems reveal high behavioral complexity and intense bioturbation in the terminal Ediacaran
inferred← citeshttps://doi.org/10.2475/001c.74874openalex-snapshot
Integrated Litho-, Chemo- and Sequence Stratigraphy of the Ediacaran Gametrail Formation Across a Shelf-Slope Transect in the Wernecke Mountains, Yukon, Canada
inferred← citeshttps://doi.org/10.3389/feart.2022.826353openalex-snapshot
What Happens Between Depositional Events, Stays Between Depositional Events: The Significance of Organic Mat Surfaces in the Capture of Ediacara Communities and the Sedimentary Rocks That Preserve Them
inferred← citeshttps://doi.org/10.51291/2377-7478.1204openalex-snapshot
Consciousness is not inherent in but emergent from life
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