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Oxygen isotope analysis of the eyes of pelagic trilobites: Testing the application of sea temperature proxies for the Ordovician

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What this work says

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

inferredcites →https://doi.org/10.1002/2016pa002928openalex-snapshot
Glacial onset predated Late Ordovician climate cooling
inferredcites →https://doi.org/10.1016/0009-2541(89)90051-xopenalex-snapshot
Geochemistry of some Ordovician and Devonian trilobite cuticles from North America
inferredcites →https://doi.org/10.1016/0016-7037(92)90143-7openalex-snapshot
and in lower Paleozoic articulate brachiopods: Implications for the isotopic composition of seawater
inferredcites →https://doi.org/10.1016/j.asd.2006.08.002openalex-snapshot
The eyes of trilobites: The oldest preserved visual system
inferredcites →https://doi.org/10.1016/j.chemgeo.2003.10.013openalex-snapshot
Carbon, oxygen and strontium isotopes in Paleozoic carbonate components: an evaluation of original seawater-chemistry proxies
inferredcites →https://doi.org/10.1016/j.chemgeo.2011.12.019openalex-snapshot
Micromorphology and differential preservation of Upper Permian brachiopod low-Mg calcite
inferredcites →https://doi.org/10.1016/j.chemgeo.2012.04.033openalex-snapshot
Biomineralisation in the Palaeozoic oceans: Evidence for simultaneous crystallisation of high and low magnesium calcite by phacopine trilobites
inferredcites →https://doi.org/10.1016/j.chemgeo.2012.10.021openalex-snapshot
Brachiopods recording seawater temperature—A matter of class or maturation?
inferredcites →https://doi.org/10.1016/j.chemgeo.2013.09.014openalex-snapshot
Oxygen isotopes and MgCO3 in brachiopod calcite and a new paleotemperature equation
inferredcites →https://doi.org/10.1016/j.chemgeo.2017.10.011openalex-snapshot
Coupling Δ47 and fluid inclusion thermometry on carbonate cements to precisely reconstruct the temperature, salinity and δ18O of paleo-groundwater in sedimentary basins
inferredcites →https://doi.org/10.1016/j.chemgeo.2017.12.026openalex-snapshot
Improving paleohydrological and diagenetic reconstructions in calcite veins and breccia of a sedimentary basin by combining Δ47 temperature, δ18Owater and U-Pb age
inferredcites →https://doi.org/10.1016/j.earscirev.2007.04.002openalex-snapshot
The oxygen isotope evolution of seawater: A critical review of a long-standing controversy and an improved geological water cycle model for the past 3.4 billion years
inferredcites →https://doi.org/10.1016/j.earscirev.2015.03.008openalex-snapshot
Temperatures and oxygen isotopic composition of Phanerozoic oceans
inferredcites →https://doi.org/10.1016/j.epsl.2012.07.021openalex-snapshot
Carbonate clumped isotope bond reordering and geospeedometry
inferredcites →https://doi.org/10.1016/j.gca.2005.11.014openalex-snapshot
13C–18O bonds in carbonate minerals: A new kind of paleothermometer
inferredcites →https://doi.org/10.1016/j.gca.2011.09.025openalex-snapshot
Defining an absolute reference frame for ‘clumped’ isotope studies of CO2
inferredcites →https://doi.org/10.1016/j.gca.2014.04.040openalex-snapshot
Temperature limits for preservation of primary calcite clumped isotope paleotemperatures
inferredcites →https://doi.org/10.1016/j.gca.2014.05.024openalex-snapshot
Carbonate clumped isotope constraints on Silurian ocean temperature and seawater δ18O
inferredcites →https://doi.org/10.1016/j.gca.2016.11.028openalex-snapshot
Calibration of the dolomite clumped isotope thermometer from 25 to 350 °C, and implications for a universal calibration for all (Ca, Mg, Fe)CO3 carbonates
inferredcites →https://doi.org/10.1016/j.gca.2017.02.025openalex-snapshot
Laboratory-grown coccoliths exhibit no vital effect in clumped isotope (Δ47) composition on a range of geologically relevant temperatures
inferredcites →https://doi.org/10.1016/j.precamres.2015.04.010openalex-snapshot
Evolution of Neoproterozoic Wonoka–Shuram Anomaly-aged carbonates: Evidence from clumped isotope paleothermometry
inferredcites →https://doi.org/10.1016/s0009-2541(99)00081-9openalex-snapshot
87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater
inferredcites →https://doi.org/10.1016/s0016-7037(02)01116-xopenalex-snapshot
Sr, C, and O isotope geochemistry of Ordovician brachiopods: a major isotopic event around the Middle-Late Ordovician transition
inferredcites →https://doi.org/10.1016/s0016-7037(97)00136-1openalex-snapshot
Paleoenvironmental changes in the Silurian indicated by stable isotopes in brachiopod shells from Gotland, Sweden
inferredcites →https://doi.org/10.1017/s0022336000027724openalex-snapshot
The most widely distributed trilobite species: Ordovician Carolinites genacinaca
inferredcites →https://doi.org/10.1017/s1755691011010097openalex-snapshot
Light guide lenses in trilobites?
inferredcites →https://doi.org/10.1029/2008pa001720openalex-snapshot
Ground‐truthing Late Ordovician climate models using the paleobiogeography of graptolites
inferredcites →https://doi.org/10.1038/srep18787openalex-snapshot
The nature of Ordovician limestone-marl alternations in the Oslo-Asker District (Norway): witnesses of primary glacio-eustasy or diagenetic rhythms?
inferredcites →https://doi.org/10.1038/srep18884openalex-snapshot
Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse
inferredcites →https://doi.org/10.1080/03115517708527766openalex-snapshot
Early Ordovician conodont and trilobite communities of Spitsbergen: influence on biogeography
inferredcites →https://doi.org/10.1080/08120098908729506openalex-snapshot
Regional thermal history of the Lennard shelf, Canning Basin, from apatite fission track analysis: Implications for the formation of Pb‐Zn ore deposits
inferredcites →https://doi.org/10.1080/08912969009386533openalex-snapshot
Primary and diagenetic microstructures in trilobite exoskeletons
inferredcites →https://doi.org/10.1080/11035898009454495openalex-snapshot
Conodonts as paleotemperature tools in Ordovician rocks of the Caledonides and adjacent areas in Scandinavia and the British Isles
inferredcites →https://doi.org/10.1111/j.1475-4983.2007.00710.xopenalex-snapshot
MAGNESIUM‐RICH INTRALENSAR STRUCTURES IN SCHIZOCHROAL TRILOBITE EYES
inferredcites →https://doi.org/10.1111/pala.12088openalex-snapshot
Microstructure and growth of the lenses of schizochroal trilobite eyes
inferredcites →https://doi.org/10.1111/sed.12427openalex-snapshot
Basin‐scale thermal and fluid flow histories revealed by carbonate clumped isotopes (Δ47) – Middle Jurassic carbonates of the Paris Basin depocentre
inferredcites →https://doi.org/10.1126/science.1155814openalex-snapshot
Did Cooling Oceans Trigger Ordovician Biodiversification? Evidence from Conodont Thermometry
inferredcites →https://doi.org/10.1126/science.1200803openalex-snapshot
The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation
inferredcites →https://doi.org/10.1126/science.230.4722.132openalex-snapshot
Life at high temperatures.
inferredcites →https://doi.org/10.1127/pala/240/1996/65openalex-snapshot
Early Ordovician trilobite taxonomy and biostratigraphy of the Emanuel Formation, Canning Basin, Western Australia
inferredcites →https://doi.org/10.1130/0016-7606(1973)84<2227:crathn>2.0.co;2openalex-snapshot
Cambrian-Ordovician Rocks Adjacent to Hinlopenstretet, North Ny Friesland, Spitsbergen
inferredcites →https://doi.org/10.1130/0016-7606(1993)105<1284:siilpb>2.3.co;2openalex-snapshot
Stable isotopes in Late Pennsylvanian brachiopods from the United States: Implications for Carboniferous paleoceanography
inferredcites →https://doi.org/10.1130/0091-7613(2002)030<0711:caosic>2.0.co;2openalex-snapshot
Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction
inferredcites →https://doi.org/10.1130/g34158.1openalex-snapshot
Original spotted patterns on Middle Devonian phacopid trilobites from western and central New York
inferredcites →https://doi.org/10.1144/0016-76492011-048openalex-snapshot
Oxygen isotope variability in conodonts: implications for reconstructing Palaeozoic palaeoclimates and palaeoceanography
inferredcites →https://doi.org/10.1666/0094-8373(1998)024[0235:itoaph]2.3.co;2openalex-snapshot
Independent testing of a paleobiological hypothesis: the optical design of two Ordovician pelagic trilobites reveals their relative paleobathymetry
inferredcites →https://doi.org/10.18261/8200049639-1975-07openalex-snapshot
Microstructure and composition of the trilobite exoskeleton
inferredcites →https://doi.org/10.2110/palo.2009.p09-101ropenalex-snapshot
CARBONATES IN SKELETON-POOR SEAS: NEW INSIGHTS FROM CAMBRIAN AND ORDOVICIAN STRATA OF LAURENTIA
inferredcites →https://doi.org/10.2475/05.2015.01openalex-snapshot
The kinetics of solid-state isotope-exchange reactions for clumped isotopes: A study of inorganic calcites and apatites from natural and experimental samples
inferredcites →https://doi.org/10.3140/bull.geosci.2007.01.027openalex-snapshot
Exoskeletal structures and ultrastructures in Lower Devonian dalmanitid trilobites of the Prague Basin (Czech Republic)
inferredcites →https://doi.org/10.5194/bg-6-1209-2009openalex-snapshot
Ion microprobe assessment of the heterogeneity of Mg/Ca, Sr/Ca and Mn/Ca ratios in Pecten maximus and Mytilus edulis (bivalvia) shell calcite precipitated at constant temperature
inferredcites →https://doi.org/10.5194/cp-10-2053-2014openalex-snapshot
Effect of the Ordovician paleogeography on the (in)stability of the climate
inferredcites →https://doi.org/10.5281/zenodo.16121878openalex-snapshot
Original mineralogy of trilobite exoskeletons
inferredcites →https://doi.org/10.5281/zenodo.16556333openalex-snapshot
Cuticular ultrastructure of the trilobite Ellipsocephalus polytomus from the Middle Cambrian of Öland, Sweden

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.4705841openalex-extracted
Modeling the Crystallographic Transformation in Shells of Mytilus Galloprovincialis During Diagenesis Through Thermal Simulation
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.120727openalex-snapshot
Isotopes of carbon and oxygen of siderite and their genetic indications for the Late Permian critical-metal tuffaceous deposits (Nb-Zr-REY-Ga) from Yunnan, southwestern China
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.106767openalex-snapshot
The thermal history of Permian carbonate strata reconstructed with clumped isotopes and U–Pb dating: Eastern Sichuan Basin, SW China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109584openalex-snapshot
δ30Si and δ18O of multiple silica phases in chert: Implications for δ30Siseawater of Darriwilian seawater and sea surface temperatures
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112523openalex-snapshot
Thermal-induced crystallographic transformation in shells of Mytilus galloprovincialis Lamarck, 1819
inferred← citeshttps://doi.org/10.1016/j.petrol.2022.111033openalex-snapshot
Organic geochemistry of Cambro-Ordovician succession of Ny Friesland, Svalbard, High Arctic Norway: Petroleum generation potential and bulk geochemical properties
inferred← citeshttps://doi.org/10.1029/2020jb020636openalex-snapshot
A Thermal Pulse Induced by a Permian Mantle Plume in the Tarim Basin, Northwest China: Constraints From Clumped Isotope Thermometry and In Situ Calcite U‐Pb Dating
inferred← citeshttps://doi.org/10.1038/s41467-021-22228-7openalex-snapshot
Reply to “Points of view in understanding trilobite eyes”
inferred← citeshttps://doi.org/10.1073/pnas.2013083118openalex-snapshot
A high-resolution record of early Paleozoic climate
inferred← citeshttps://doi.org/10.1098/rsos.250478openalex-snapshot
Exceptionally preserved Cretaceous crabs provide novel insights into the fossilization of arthropod compound eyes
inferred← citeshttps://doi.org/10.1111/bre.12324openalex-snapshot
Thermal and exhumation histories of the northern subalpine chains (Bauges and Bornes—France): Evidence from forward thermal modeling coupling clay mineral diagenesis, organic maturity and carbonate clumped isotope (Δ 47 ) data
inferred← citeshttps://doi.org/10.3390/min15070699openalex-snapshot
Genesis and Evolution of the Qieliekeqi Siderite Deposit in the West Kunlun Orogen: Constraints from Geochemistry, Zircon U–Pb Geochronology, and Carbon–Oxygen Isotopes
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