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Silica‐rich seawater in the early Cambrian: Sedimentological evidence from bedded cherts

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

inferredcites →https://doi.org/10.1002/2014gc005595openalex-snapshot

Germanium/silicon of the Ediacaran-Cambrian Laobao cherts: Implications for the bedded chert formation and paleoenvironment interpretations

inferredcites →https://doi.org/10.1007/s12583-017-0960-0openalex-snapshot

New Siliceous Microfossils from the Terreneuvian Yanjiahe Formation, South China: The Possible Earliest Radiolarian Fossil Record

inferredcites →https://doi.org/10.1016/0016-7037(92)90303-zopenalex-snapshot

The silica cycle in the Precambrian

inferredcites →https://doi.org/10.1016/b978-0-08-095975-7.00705-1openalex-snapshot

Formation and Geochemistry of Precambrian Cherts

inferredcites →https://doi.org/10.1016/j.chemgeo.2008.10.016openalex-snapshot

Hydrothermal venting activities in the Early Cambrian, South China: Petrological, geochronological and stable isotopic constraints

inferredcites →https://doi.org/10.1016/j.chemgeo.2020.119787openalex-snapshot

Silicification and Si cycling in a silica-rich ocean during the Ediacaran-Cambrian transition

inferredcites →https://doi.org/10.1016/j.jseaes.2008.07.003openalex-snapshot

Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin, Northwest China: Implications for depositional setting and tectonic history

inferredcites →https://doi.org/10.1016/j.marpetgeo.2012.08.006openalex-snapshot

Primary silica precipitate at the Precambrian/Cambrian boundary in the South Oman Salt Basin, Sultanate of Oman

inferredcites →https://doi.org/10.1016/j.palaeo.2004.12.017openalex-snapshot

Implications for the history of Cenozoic opal deposition from a quantitative model

inferredcites →https://doi.org/10.1016/j.palaeo.2007.03.016openalex-snapshot

Trace element chemostratigraphy of two Ediacaran–Cambrian successions in South China: Implications for organosedimentary metal enrichment and silicification in the Early Cambrian

inferredcites →https://doi.org/10.1016/j.precamres.2015.03.006openalex-snapshot

Diagenetic barite deposits in the Yurtus Formation in Tarim Basin, NW China: Implications for barium and sulfur cycling in the earliest Cambrian

inferredcites →https://doi.org/10.1016/j.precamres.2019.105438openalex-snapshot

The Ediacaran-Cambrian rise of siliceous sponges and development of modern oceanic ecosystems

inferredcites →https://doi.org/10.1038/nature10969openalex-snapshot

Formation of the ‘Great Unconformity’ as a trigger for the Cambrian explosion

inferredcites →https://doi.org/10.1038/s41467-017-00586-5openalex-snapshot

Late Neoproterozoic seawater oxygenation by siliceous sponges

inferredcites →https://doi.org/10.1080/00206814.2014.968885openalex-snapshot

Submarine silica-rich hydrothermal activity during the earliest Cambrian in the Tarim Basin, Northwest China

inferredcites →https://doi.org/10.1080/00206814.2018.1474498openalex-snapshot

The unconformity-related palaeokarst in the uppermost Ediacaran carbonate rocks in the northwestern Tarim Block, NW China: implication for sedimentary evolution during the Ediacaran–Cambrian transition

inferredcites →https://doi.org/10.1086/320794openalex-snapshot

Secular Distribution of Biogenic Silica through the Phanerozoic: Comparison of Silica‐Replaced Fossils and Bedded Cherts at the Series Level

inferredcites →https://doi.org/10.1111/brv.12090openalex-snapshot

Giving the early fossil record of sponges a squeeze

inferredcites →https://doi.org/10.1111/gbi.12236openalex-snapshot

Paleoecology and paleoceanography of the Athel silicilyte, Ediacaran–Cambrian boundary, Sultanate of Oman

inferredcites →https://doi.org/10.1111/j.1365-3091.1985.tb00490.xopenalex-snapshot

Sedimentology of cherts in the Early Proterozoic Wishart Formation, Quebec‐Newfoundland, Canada

inferredcites →https://doi.org/10.1111/j.1475-4983.2005.00484.xopenalex-snapshot

BASAL CAMBRIAN MICROFOSSILS FROM THE YURTUS AND XISHANBLAQ FORMATIONS (TARIM, NORTH-WEST CHINA): SYSTEMATIC REVISION AND BIOSTRATIGRAPHIC CORRELATION OF MICRHYSTRIDIUM-LIKE ACRITARCHS

inferredcites →https://doi.org/10.1111/sed.12173openalex-snapshot

Origin and variability of a terminal Proterozoic primary silica precipitate, Athel Silicilyte, South Oman Salt Basin, Sultanate of Oman

inferredcites →https://doi.org/10.1126/science.aad5787openalex-snapshot

Continental arc volcanism as the principal driver of icehouse-greenhouse variability

inferredcites →https://doi.org/10.1130/0091-7613(1992)020<0271:dfobce>2.3.co;2openalex-snapshot

Diagenetic formation of bedded chert: Evidence from chemistry of the chert-shale couplet

inferredcites →https://doi.org/10.1130/0091-7613(1994)022<0207:psoade>2.3.co;2openalex-snapshot

Pure siliceous ooze, a diagenetic environment for early chert formation

inferredcites →https://doi.org/10.1130/0091-7613(1998)026<0899:sssite>2.3.co;2openalex-snapshot

Siliceous sponge spicules in the Early Cambrian chert-phosphorite member of the Lower Tal Formation, Krol belt, Lesser Himalaya

inferredcites →https://doi.org/10.1130/0091-7613(2003)031<0319:pamsrs>2.0.co;2openalex-snapshot

Paleozoic and Mesozoic silica-rich seawater: Evidence from hematitic chert (jasper) deposits

inferredcites →https://doi.org/10.1130/b25555.1openalex-snapshot

Secular change in the Precambrian silica cycle: Insights from chert petrology

inferredcites →https://doi.org/10.1130/b26328.1openalex-snapshot

An iron shuttle for deepwater silica in Late Archean and early Paleoproterozoic iron formation

inferredcites →https://doi.org/10.1130/b30346.1openalex-snapshot

The earliest Cambrian record of animals and ocean geochemical change

inferredcites →https://doi.org/10.1130/g25057a.1openalex-snapshot

Biogenic silica and chert in the Pacific Ocean

inferredcites →https://doi.org/10.1130/g30101a.1openalex-snapshot

An early ecosystem of Archean tidal microbial mats (Moodies Group, South Africa, ca. 3.2 Ga)

inferredcites →https://doi.org/10.1130/g35187.1openalex-snapshot

Primary silica granules—A new mode of Paleoarchean sedimentation

inferredcites →https://doi.org/10.1130/g35886.1openalex-snapshot

Cambrian transgression and radiation linked to an Iapetus-Pacific oceanic connection?

inferredcites →https://doi.org/10.1130/g36363.1openalex-snapshot

Seafloor silicification and hardground development during deposition of 2.5 Ga banded iron formations

inferredcites →https://doi.org/10.1130/g38542.1openalex-snapshot

Exceptional preservation of soft-bodied Ediacara Biota promoted by silica-rich oceans

inferredcites →https://doi.org/10.1130/g45560.1openalex-snapshot

Evidence from laminated chert in banded iron formations for deposition by gravitational settling of iron-silicate muds

inferredcites →https://doi.org/10.1130/g46162.1openalex-snapshot

Evidence for anoxic shallow oceans at 2.45 Ga: Implications for the rise of oxygenic photosynthesis

inferredcites →https://doi.org/10.1144/jmpaleo2013-003openalex-snapshot

On the Lower Cambrian biotic and geochemical record of the Hetang Formation (Yangtze Platform, south China): evidence for biogenic silica and possible presence of Radiolaria

inferredcites →https://doi.org/10.1144/sp286.10openalex-snapshot

First Early Cambrian Radiolaria

inferredcites →https://doi.org/10.1146/annurev-marine-121211-172346openalex-snapshot

The World Ocean Silica Cycle

inferredcites →https://doi.org/10.1666/07-147r.1openalex-snapshot

Basal Cambrian microfossils from the Yangtze Gorges area (South China) and the Aksu area (Tarim block, northwestern China)

inferredcites →https://doi.org/10.2307/3514743openalex-snapshot

Secular change in chert distribution; a reflection of evolving biological participation in the silica cycle

inferredcites →https://doi.org/10.3389/fmars.2017.00397openalex-snapshot

Biosilicification Drives a Decline of Dissolved Si in the Oceans through Geologic Time

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

inferred← citeshttps://doi.org/10.2139/ssrn.4793076openalex-extracted

Anatomy on Depositional Facies And Evolution of Sponge-Microbial-Constructed Carbonate Platforms In The Lower Cambrian (Stage 3), Tarim Basin, China

inferred← citeshttps://doi.org/10.1007/s11631-026-00872-4openalex-snapshot

Whole-rock geochemical constraints on origin of ferruginous chert and associated rocks from the Neoproterozoic Buem Structural Unit, Eastern Ghana: Implications for hydrothermal activity and tectonic setting

inferred← citeshttps://doi.org/10.1007/s13146-025-01120-1openalex-snapshot

Depositional evolution and carbon isotopic oscillations of the Lower Cambrian Yuertusi Formation in Western Tarim Basin (NW China)

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2023.121631openalex-snapshot

Diagenetic effect on barium isotope compositions of barites in the lower Cambrian successions

inferred← citeshttps://doi.org/10.1016/j.jop.2024.07.002openalex-snapshot

Geochemistry of cherts from the northern Jiangxi region, South China: Implication for paleoenvironment

inferred← citeshttps://doi.org/10.1016/j.jseaes.2023.105623openalex-snapshot

The coupled evolution of depositional systems and paleo-redox conditions was recorded in terminal Ediacaran sedimentary succession in the Tarim Block, NW China

inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2022.105991openalex-snapshot

Trace elements and stable isotopic geochemistry of two sedimentary sections in the lower Cambrian strata from the Tarim Basin, northwest China: Implications for silicification and biological evolution

inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.106929openalex-snapshot

Dolomitization history and fluid evolution of end-ediacaran multi-phase dolomites from the near-surface to deep burial depths in the tarim craton, northwestern China

inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.106957openalex-snapshot

Depositional facies and evolution of sponge-microbial-constructed carbonate platforms in the lower Cambrian (Stage 3), Tarim basin, China: Understanding from anatomy

inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112506openalex-snapshot

Synchrotron-based P K-edge XANES spectroscopy reveals the transition of phosphorus cycling in the early Cambrian ocean

inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113411openalex-snapshot

Carbonate platform evolution in response to carbonate factory change during the Cambrian Explosion (Age 3), NW Tarim Basin, China

inferred← citeshttps://doi.org/10.1016/j.sedgeo.2023.106571openalex-snapshot

Upwelling-driven biogenic silica accumulation in the Yangtze Sea, South China during Late Ordovician to Early Silurian time: A possible link with the global climatic transitions

inferred← citeshttps://doi.org/10.1130/b37869.1openalex-snapshot

Environmental controls on Early Cambrian macroevolution: Insights from the Tarim Basin, Northwest China

inferred← citeshttps://doi.org/10.1306/01242422096openalex-snapshot

Comparison of silica diagenesis between the lower Cambrian and lower Silurian shale reservoirs in the middle–upper Yangtze platform (southern China)

inferred← citeshttps://doi.org/10.2110/palo.2025.035openalex-snapshot

TAPHONOMY AND PALEOENVIRONMENTAL SIGNIFICANCE OF SILICIFIED CYANOBACTERIAL FOSSILS IN THE EARLY CAMBRIAN HARKLESS FORMATION, NEVADA, USA

inferred← citeshttps://doi.org/10.3103/s0145875223010155openalex-snapshot

Conditions for the Formation of Siliceous Rocks of the Lower and Middle Cambrian in the Southeast of the Siberian Platform

inferred← citeshttps://doi.org/10.33623/0579-9406-2022-6-71-82openalex-snapshot

Conditions for the formation of siliceous rocks of the Lower-Middle Cambrian in the southeast of the Siberian Platform

inferred← citeshttps://doi.org/10.3390/min14010035openalex-snapshot

Early Dolomitization Mechanism of the Upper Ediacaran Qigebrak Formation, Northwestern Tarim Basin: Evidence from Petrography, Rare Earth Elements, and Clumped Isotope

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