The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Stable Isotopes in a Mollusk Shell: Detection of Upwelling Events
Abstract
The California mussel Mytilus californianus records with high fidelity annual temperature variations of nearshore waters in the oxygen isotope composition of its shell. The onset and termination of upwelling events (and metabolic activity) are recorded in the associated carbon isotope signal, and the magnitude and timing of upwelling can be estimated. The method has implications for studying the history of upwelling and the life history of living and fossil mollusks and for analyzing shell midden deposits.
Overview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
In the citing paper
“Mineral precipitation at low temperatures are enriched in 18 O while minerals formed at high temperatures show less 18 O enrichment [11]”
From Isotopes (13C and 18O) Geochemistry of Lower Triassic Montney Formation, Northeastern British Columbia, Western Canada (2017) · cites this paper as [11]
In the citing paper
“they are established methods for studying dolomitization and diagenesis in carbonates [11,12].”
From Isotopes (13C and 18O) Geochemistry of Lower Triassic Montney Formation, Northeastern British Columbia, Western Canada (2017) · cites this paper as [11]
In the citing paper
“Unaltered silicate rocks are enriched in δ 18 O relative to seawater by ~5.7‰ [11].”
From Isotopes (13C and 18O) Geochemistry of Lower Triassic Montney Formation, Northeastern British Columbia, Western Canada (2017) · cites this paper as [11]
Citations
Cites
Epstein, S., & Lowenstam, H. A. (1953) · The Journal of Geology · doi:10.1086/626110 · Cited by 123
Research works printed but not linked: 36
- 10.1126/science.191.4232.1131 · DOI
- Bakun, A, NOAA Marine Resources Monitoring. Assessment, and Prediction (MARMAP) Contribution 104: 12 (1976).
- BERGER, W.H., PLANKTONIC FORAMINIFERA - SELECTIVE SOLUTION AND PALEOCLIMATIC INTERPRETATION, DEEP-SEA RESEARCH 15: 31 (1968).
- BERGER, W.H., UPWELLING OFF NORTHWEST AFRICA - HOLOCENE DECREASE AS SEEN IN CARBON ISOTOPES AND SEDIMENTOLOGICAL INDICATORS, OCEANOLOGICA ACTA 1: 3 (1978).
- BERGER, W.H., STABLE ISOTOPES IN DEEP-SEA CARBONATES - BOX CORE ERDC-92, WEST EQUATORIAL PACIFIC, OCEANOLOGICA ACTA 1: 203 (1978).
- 10.1126/science.197.4303.563 · DOI
- Craig, H., 2nd Conference, Stable Isotopes in Oceanographic Studies and Paleotemperatures: 9 (1965).
- Craig, H., 2nd Conference, Stable Isotopes in Oceanographic Studies and Paleotemperatures: 161 (1965).
- DIESTERHAASS, L, METEOR FORSCHUNGSERGEBNISSE. REIHE C 16: 19 (1973).
- DODD, J.R., ENVIRONMENTAL CONTROL OF STRONTIUM AND MAGNESIUM IN MYTILUS, GEOCHIMICA ET COSMOCHIMICA ACTA 29: 385 (1965). · DOI
- DODD, J.R., ENVIRONMENTALLY CONTROLLED VARIATION IN THE SHELL STRUCTURE OF A PELECYPOD SPECIES, JOURNAL OF PALEONTOLOGY 38: 1065 (1964).
- EBER, L.E., CALCOFI ATLAS: 80 (1977).
- EMILIANI, C, OXYGEN ISOTOPIC ANALYSIS OF SOME MOLLUSCAN SHELLS FROM FOSSIL LITTORAL DEPOSITS OF PLEISTOCENE AGE, AMERICAN JOURNAL OF SCIENCE 262: 107 (1964). · DOI
- EMRICH, K, CARBON ISOTOPE FRACTIONATION DURING PRECIPITATION OF CALCIUM CARBONATE, EARTH AND PLANETARY SCIENCE LETTERS 8: 363 (1970). · DOI
- HEATH, G.R., GEOLOGICAL SOCIETY OF AMERICA MEMOIR 145: 393 (1976). · DOI
- KEITH, M.L., GEOCHIMICA ET COSMOCHIMICA ACTA 28: 1787 (1964). · DOI
- KEITH, M.L., MAR GEOL 3: 115 (1965). · DOI
- KENNETT, J.P., CENOZOIC EVOLUTION OF ANTARCTIC GLACIATION, CIRCUM-ANTARCTIC OCEAN, AND THEIR IMPACT ON GLOBAL PALEOCEANOGRAPHY, JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES 82: 3843 (1977). · DOI
- KROOPNICK, P, DISSOLVED O2-CO2-C-13 SYSTEM IN EASTERN EQUATORIAL PACIFIC, DEEP-SEA RESEARCH 21: 211 (1974).
- Kroopnick, P., Journal of Geophysical Research 75: 7668 (1970). · DOI
- KU, T.L., URANIUM-SERIES AGE OF UPPER PLEISTOCENE NESTOR TERRACE, SAN-DIEGO, CALIFORNIA, GEOLOGICAL SOCIETY OF AMERICA BULLETIN 85: 1713 (1974). · DOI
- LLOYD, R.M., J GEOL 72: 84 (1967).
- LONGINELLI, A, BOLLETTINO DELLA SOCIETA PALEONTOLOGICA ITALIANA 1: 52 (1962).
- LOWENSTAM, H.A., MINERALOGY, O-18/O-16 RATIOS, AND STRONTIUM AND MAGNESIUM CONTENTS OF RECENT AND FOSSIL BRACHIOPODS AND THEIR BEARING ON THE HISTORY OF THE OCEANS, JOURNAL OF GEOLOGY 69: 241 (1961). · DOI
- MCLEAN, J.H., MARINE SHELLS SO CAL: 66 (1978).
- MOLINACRUZ, A, GLACIAL EASTERN BOUNDARY CURRENT ALONG ATLANTIC EURAFRICAN CONTINENTAL-MARGIN, DEEP-SEA RESEARCH 25: 337 (1978). · DOI
- PASTOURET, L, LATE QUATERNARY CLIMATIC CHANGES IN WESTERN TROPICAL AFRICA DEDUCED FROM DEEP-SEA SEDIMENTATION OFF NIGER DELTA, OCEANOLOGICA ACTA 1: 217 (1978).
- REID, J.L., CALIFORNIA COOPERATIVE OCEANIC FISHERIES INVESTIGATIONS REPORT: 28 (1958).
- SHACKLETON, N.J., OXYGEN ISOTOPE ANALYSIS AS A MEANS OF DETERMINING SEASON OF OCCUPATION OF PREHISTORIC MIDDEN SITES, ARCHAEOMETRY 15: 133 (1973). · DOI
- THIEDE, J, METEOR FORSCHUNGSERGEBNISSE. REIHE C 28: 1 (1977).
- 10.1126/science.194.4268.942 · DOI
- TOURTELOT, H.A., DISTRIBUTION OF OXYGEN AND CARBON ISOTOPES IN FOSSILS OF LATE CRETACEOUS AGE, WESTERN INTERIOR REGION OF NORTH AMERICA, GEOLOGICAL SOCIETY OF AMERICA BULLETIN 80: 1903 (1969). · DOI
- UREY, H.C., MEASUREMENT OF PALEOTEMPERATURES AND TEMPERATURES OF THE UPPER CRETACEOUS OF ENGLAND, DENMARK, AND THE SOUTHEASTERN UNITED-STATES, GEOLOGICAL SOCIETY OF AMERICA BULLETIN 62: 399 (1951). · DOI
- VALENTINE, J.W., HABITATS AND SOURCES OF PLEISTOCENE MOLLUSKS AT TORREY-PINES PARK, CALIFORNIA, ECOLOGY 41: 161 (1960). · DOI
- VALENTINE, J.W., ISOTOPIC AND ZOOGEOGRAPHIC PALEOTEMPERATURES OF CALIFORNIAN PLEISTOCENE MOLLUSCA, SCIENCE 132: 810 (1960). · DOI
- WILLIAMS, D.F., CARBON ISOTOPIC COMPOSITIONS OF RECENT PLANKTONIC FORAMINIFERA OF INDIAN-OCEAN, EARTH AND PLANETARY SCIENCE LETTERS 36: 391 (1977). · DOI
Cited by
Sorted by citations
Egbobawaye, E. I. (2017) · Natural Science · doi:10.4236/ns.2017.910034 · Cited by 1
“Mineral precipitation at low temperatures are enriched in (18)O while minerals formed at high temperatures show less (18)O enrichment [11]; and 2) dolomitized Montney Formation has mainly undergone eogenetic stage of diagenesis.”
BackgroundMethodInfluential
Metadata
- Authors
- Killingley, J. S., & Berger, W. H.
- Affiliations
- Scripps Institution of Oceanography (US)
- Venue
- Science
- Published
- 1979-07-13
- Volume
- 205
- Issue
- 4402
- Pages
- 186-188
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W1991746792
- Cited by
- 193
- References
- 1
- Citations by year
- 2026: 5 · 2025: 2 · 2024: 2 · 2023: 2 · 2022: 4 · 2021: 5 · 2020: 5 · 2019: 5 · 2018: 5 · 2017: 5 · 2016: 4 · 2015: 6 · 2014: 1 · 2013: 9 · 2012: 11
- FWCI
- 5.22
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Environmental Science › Ecology › Isotope Analysis in Ecology
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Life Sciences › Agricultural and Biological Sciences › Aquatic Science › Marine and fisheries research
- Keywords
- stable isotopes, mollusk shells, Mytilus californianus, upwelling, oxygen isotopes, carbon isotopes, paleoclimate, metabolic activity, annual temperature variation, California Current
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review