Bioturbation and directionality in Earth's carbon isotope record across the Neoproterozoic–Cambrian transition

No abstract is available for this paper.

• Publication year

  2018

• Venue

  Geobiology

• Publication date

  2018-05-01

• Fields of study

  Medicine, Geology

• Identifiers
  DOI 10.1111/gbi.12277PMID 29498810
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar, PubMed

• No claims are published for this paper.

• No concepts are published for this paper.

• Book Review: The trace-fossil record of major evolutionary events.

  2020cited by this paper
• Transient deep-water oxygenation in the early Cambrian Nanhua Basin, South China

  2017cited by this paper
• A model for the decrease in amplitude of carbon isotope excursions across the Phanerozoic

  2017cited by this paper
• A model for microbial phosphorus cycling in bioturbated marine sediments: Significance for phosphorus burial in the early Paleozoic

  2016cited by this paper
• Marine anoxia and delayed Earth system recovery after the end-Permian extinction

  2016cited by this paper
• A statistical analysis of the carbon isotope record from the Archean to Phanerozoic and implications for the rise of oxygen

  2015cited by this paper
• The geochemistry of carbonate diagenesis: The past, present and future

  2015cited by this paper
• Protracted development of bioturbation through the early Palaeozoic Era

  2015cited by this paper
• Environmental upheavals of the Ediacaran period and the Cambrian “explosion” of animal life

  2015cited by this paper
• Assessment of Density Variations of Marine Sediments with Ocean and Sediment Depths

  2014cited by this paper
• Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event.

  2014cited by this paper
• Stabilization of the coupled oxygen and phosphorus cycles by the evolution of bioturbation

  2014influential reference
• Widespread delayed mixing in early to middle Cambrian marine shelfal settings

  2014cited by this paper
• Decoupling of body-plan diversification and ecological structuring during the Ediacaran–Cambrian transition: evolutionary and geobiological feedbacks

  2014cited by this paper
• Hidden cycle of dissolved organic carbon in the deep ocean

  2014cited by this paper
• Interpreting carbonate and organic carbon isotope covariance in the sedimentary record

  2014cited by this paper
• Evidence for Cnidaria-like behavior in ca. 560 Ma Ediacaran Aspidella

  2013cited by this paper
• Authigenic Carbonate and the History of the Global Carbon Cycle

  2013influential reference
• The oldest evidence of bioturbation on Earth: COMMENT

  2013cited by this paper
• Carbon Cycle Makeover

  2013cited by this paper
• Carbon isotopes and lipid biomarkers from organic‐rich facies of the Shuram Formation, Sultanate of Oman

  2013cited by this paper
• What is bioturbation? The need for a precise definition for fauna in aquatic sciences

  2012cited by this paper
• atmosphere and ocean Carbon isotope excursions and the oxidant budget of the Ediacaran

  2012cited by this paper
• Uncovering the Neoproterozoic carbon cycle

  2012cited by this paper
• The oldest evidence of bioturbation on Earth

  2012cited by this paper
• Chapter 11 – Carbon Isotope Stratigraphy

  2012influential reference
• Towards a quantitative understanding of the late Neoproterozoic carbon cycle

  2011influential reference
• The Cambrian Conundrum: Early Divergence and Later Ecological Success in the Early History of Animals

  2011cited by this paper
• Geochemical evidence for widespread euxinia in the Later Cambrian ocean

  2011cited by this paper
• Enigmatic origin of the largest-known carbon isotope excursion in Earth's history

  2011cited by this paper
• First evidence for locomotion in the Ediacara biota from the 565 Ma Mistaken Point Formation, Newfoundland

  2010cited by this paper
• A burial diagenesis origin for the Ediacaran Shuram–Wonoka carbon isotope anomaly

  2010cited by this paper
• Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish

  2010cited by this paper
• First evidence for locomotion in the Ediacara biota from the 565 Ma Mistaken Point Formation, Newfou

  2010cited by this paper
• Oxygenation of the ocean and sediments: Consequences for the seafloor carbonate factory

  2009cited by this paper
• The late Precambrian greening of the Earth

  2009cited by this paper
• Effects of hypoxia on animal burrow construction and consequent effects on sediment redox profiles

  2009cited by this paper
• Isotopic Constraints on the Late Archean Carbon Cycle from the Transvaal Supergroup along the Western Margin of the Kaapvaal Craton, South Africa

  2009cited by this paper
• Animal evolution, bioturbation, and the sulfate concentration of the oceans

  2009cited by this paper
• Carbon isotope excursions and the oxidant budget of the Ediacaran atmosphere and ocean

  2008cited by this paper
• Imaging Oxygen Distribution in Marine Sediments. The Importance of Bioturbation and Sediment Heterogeneity

  2008cited by this paper
• Lifetimes and time scales in atmospheric chemistry

  2007influential reference
• A synthesis of global particle export from the surface ocean and cycling through the ocean interior and on the seafloor

  2007cited by this paper
• Ocean Biogeochemical Dynamics

  2007influential reference
• Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2

  2007influential reference
• Bioturbation: a fresh look at Darwin's last idea.

  2006cited by this paper
• Geobiology and the fossil record: eukaryotes, microbes, and their interactions

  2005cited by this paper
• Empirical and mechanistic models for the particle export ratio

  2005cited by this paper
• COPSE: a new model of biogeochemical cycling over Phanerozoic time

  2004influential reference
• New insights into the burial history of organic carbon on the early Earth

  2004influential reference
• The rates of sediment-water exchange of oxygen and sediment bioturbation in Lough Neagh, Northern Ireland

  2004cited by this paper
• A 400-year record of environmental change in an euxinic fjord as revealed by the sedimentary biomarker record

  2004cited by this paper
• An alternative model for positive shifts in shallow‐marine carbonate δ13C and δ18O

  2003cited by this paper
• Charles Darwin, earthworms and the natural sciences: various lessons from past to future

  2003cited by this paper
• Dynamics of the Neoproterozoic carbon cycle

  2003cited by this paper
• Biogeochemical constraints on the Triassic‐Jurassic boundary carbon cycle event

  2002cited by this paper
• The oxygen geochemical cycle: dynamics and stability

  2002influential reference
• Carbon to phosphorus ratios in sediments: Implications for nutrient cycling

  2001influential reference
• The Cambrian Substrate Revolution

  2000cited by this paper
• Redfield revisited: 2. What regulates the oxygen content of the atmosphere?

  2000influential reference
• Evolution of the Sr and C Isotope Composition of Cambrian Oceans

  2000cited by this paper
• Organic matter diagenesis at the oxic/anoxic interface in coastal marine sediments, with emphasis on the role of burrowing animals

  2000cited by this paper
• Biomat-related lifestyles in the Precambrian

  1999influential reference
• Interpreting carbon-isotope excursions: carbonates and organic matter

  1999influential reference
• THE ABUNDANCE OF 13C IN MARINE ORGANIC MATTER AND ISOTOPIC FRACTIONATION IN THE GLOBAL BIOGEOCHEMICAL CYCLE OF CARBON DURING THE PAST 800 MA

  1999cited by this paper
• The Impact of Bioturbation on Infaunal Ecology and Evolution During the Proterozoic-Cambrian Transition

  1999cited by this paper
• A Practical Guide to Wavelet Analysis.

  1998cited by this paper
• Molecular indicators of diagenetic status in marine organic matter

  1997cited by this paper
• Empirical relationships for use in global diagenetic models

  1997cited by this paper
• Niche Construction

  1996cited by this paper
• Benthic phosphorus regeneration, net primary production, and ocean anoxia: A model of the coupled marine biogeochemical cycles of carbon and phosphorus

  1994cited by this paper
• Bioturbation and remineralization of sedimentary organic matter: effects of redox oscillation☆

  1994cited by this paper
• Evidence for enhanced phosphorus regeneration from marine sediments overlain by oxygen depleted waters

  1994cited by this paper
• An introduction to marine biogeochemistry

  1993influential reference
• Influence of water column anoxia on the burial and preservation of carbon and phosphorus in marine shales

  1993cited by this paper
• Organic Matter Oxidation in Marine Sediments

  1993influential reference
• Description and analysis of bioturbation and ichnofabric

  1993cited by this paper
• 14C activity of dissolved organic carbon fractions in the north-central Pacific and Sargasso Sea

  1992cited by this paper
• Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levels.

  1992influential reference
• The oxygen content of ocean bottom waters, the burial efficiency of organic carbon, and the regulation of atmospheric oxygen.

  1991influential reference
• Relation between sedimentation rate and burial of organic phosphorus and organic carbon in marine sediments

  1990cited by this paper
• Microstructure of diffusive boundary layers and the oxygen uptake of the sea floor

  1990cited by this paper
• Geochemistry of Precambrian carbonates: I. Archean hydrothermal systems

  1989cited by this paper
• Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States

  1988cited by this paper
• Radiocarbon in dissolved organic matter in the central North Pacific Ocean

  1987cited by this paper
• VERTEX: carbon cycling in the northeast Pacific

  1987cited by this paper
• The partitioning of organic carbon fluxes and sedimentary organic matter decomposition rates in the ocean

  1983cited by this paper
• Wave propagation and sampling theory—Part I: Complex signal and scattering in multilayered media

  1982cited by this paper
• The rates of sediment-water exchange of oxygen and sediment bioturbation in Lough Neagh, Northern Ireland

  1982cited by this paper
• Seasonality and Interaction of Biogenic and Lithogenic Particulate Flux at the Panama Basin

  1982cited by this paper
• Isotope signatures associated with early meteoric diagenesis

  1982cited by this paper
• A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature

  1981cited by this paper
• Seasonal change in the flux of organic carbon to the deep Sargasso Sea

  1980cited by this paper
• Model calculations for the terrestrial carbon cycle: carbon isotope geochemistry and evolution of photosynthetic oxygen

  1975cited by this paper
• THE GEOCHEMISTRY OF THE STABLE CARBON ISOTOPES

  1953cited by this paper

• The significance of paleoenvironmental conditions and microbial activities in the spatiotemporal distribution of the ‘Orsten’-type biota: Insights from the lower Cambrian of South China

  2026cites this paper
• The paleoenvironmental evolution of the Cambrian Miaolingian Epoch in South China

  2025cites this paper
• Early colonization of the deep-sea bottom—The protracted build-up of an ecosystem

  2025cites this paper
• Advent of three-dimensional sediment exploration reveals Ediacaran-Cambrian ecosystem transition

  2025cites this paper
• Cascading oxygen loss shoreward in the oceans: Insights from the Cambrian SPICE event

  2024cites this paper
• Terminal Ediacaran–Terreneuvian revolutions in Siberia

  2024cites this paper
• The Jurassic–Cretaceous boundary in the Kurovice section (Southern Moravia, Czech Republic): trace fossils, stable isotopes, and magnetic susceptibility

  2023cites this paper
• Life on the Edge: The Cambrian Marine Realm and Oxygenation

  2023cites this paper
• Digging Deeper: Bioturbation increases the preserved sulfur isotope fractionation

  2023cites this paper
• Environmental and temporal patterns in bioturbation in the Cambrian–Ordovician of Western Newfoundland

  2023cites this paper
• Sea-level changes control coastal organic carbon burial in the southern East China Sea during the late MIS 3

  2023cites this paper
• Assessing the expansion of the Cambrian Agronomic Revolution into fan-delta environments

  2022cites this paper
• Pannotia: To be or not to be?

  2022cites this paper
• SUPERIMPOSED ALLOGENIC AND BIOLOGICAL CONTROLS ON SILICICLASTIC ARCHITECTURE: AN EARLY MISSISSIPPIAN (VISEAN) EXAMPLE FROM TROPICAL LAURUSSIA

  2022cites this paper
• SPOTLIGHTTHE ARROWS IN ORGANISM-SUBSTRATE INTERACTIONS

  2021cites this paper
• Bioturbation of Thalassinoides from the Lower Cambrian Zhushadong Formation of Dengfeng area, Henan Province, North China

  2021cites this paper
• New insights into the early evolution of horizontal spiral trace fossils and the age of the Brioverian series (Ediacaran–Cambrian) in Brittany, NW France

  2021cites this paper
• Snowballs in Africa: sectioning a long-lived Neoproterozoic carbonate platform and its bathyal foreslope (NW Namibia)

  2021cites this paper
• Bioturbation feedbacks on the phosphorus cycle

  2021cites this paper
• A largely invariant marine dissolved organic carbon reservoir across Earth's history

  2021cites this paper
• The interplay of environmental constraints and bioturbation on matground development along the marine depositional profile during the Ordovician Radiation

  2021cites this paper
• What controls the duration and intensity of ocean anoxic events in the Paleozoic and the Mesozoic?

  2021cites this paper
• The evolution of complex life and the stabilization of the Earth system

  2020cites this paper
• Pannotia under prosecution

  2020cites this paper
• The rise and early evolution of animals: where do we stand from a trace-fossil perspective?

  2020cites this paper
• Evolutionary synchrony of Earth’s biosphere and sedimentary-stratigraphic record

  2020cites this paper
• BPOP-v1 model: exploring the impact of changes in the biological pump on the shelf sea and ocean nutrient and redox state

  2019cites this paper
• Integrated records of environmental change and evolution challenge the Cambrian Explosion

  2019cites this paper
• Atmosphere–ocean oxygen and productivity dynamics during early animal radiations

  2019cites this paper
• Effects of bioturbation on carbon and sulfur cycling across the Ediacaran–Cambrian transition at the GSSP in Newfoundland, Canada

  2018cites this paper
• Provenance and geochemical variations across the Ediacaran–Cambrian transition in the Soltanieh Formation, Alborz Mountains, Iran

  2018cites this paper
• The chemical evolution of the Proterozoic biosphere

  2018cites this paper
• Smith ScholarWorks Smith ScholarWorks

  year unknowncites this paper