CoChat
Sign Up
Cited by 13

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

The California Current System as a transmitter of millennial scale climate change on the northeastern Pacific margin from 10 to 50 ka: SST RECORD 10-50 KA IN THE NORTH PACIFIC

Taylor, M. A., Hendy, I. L., Pak, D. K.·2015·Paleoceanography
DOI 10.1002/2014pa002738
Open this paper in CoChat — free account

Overview

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

Integrity signals

Registry

Crossref · 10.1002/2014pa002738

Cites

1 of 1 references verified0 citation errors · 0 not checkable

Statistics

Verification

Claims the paper makes

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

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?

  • The regional signature of ocean temperatures in the Northeast Pacific during deglaciation has been linked to the strength of the California Current driven by movement of the Intertropical Convergence Zone, in turn linked to the growth and decay of the Laurentide and Cordilleran ice sheets.

    “The regional signature of ocean temperatures in the Northeast Pacific during deglaciation has been linked to the strength of the California Current driven by movement of the Intertropical Convergence Zone, in turn linked to the growth and decay of the Laurentide and Cordilleran ice sheets (Taylor et al., 2015).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Taylor et al., 2015

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

The self-check needs the paper’s full text.

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 85

  1. Antonov, 2006, World Ocean Atlas 2005, Volume 2: Salinity, 182
  2. Auad, 2011, The California Current System in relation to the Northeast Pacific Ocean circulation, Prog. Oceanogr., 91, 576, 10.1016/j.pocean.2011.09.004 · DOI
  3. Barker, 2003, A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry, Geochem. Geophys. Geosyst., 4, 10.1029/2003GC000559 · DOI
  4. Beghin, 2014, Interdependence of the growth of the Northern Hemisphere ice sheets during the last glaciation: The role of atmospheric circulation, Clim.Past, 10, 345, 10.5194/cp-10-345-2014 · DOI
  5. Behl, 1996, Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr, Nature, 379, 243, 10.1038/379243a0 · DOI
  6. Bemis, 1998, Reevalution of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations, Paleoceanography, 13, 150, 10.1029/98PA00070 · DOI
  7. Bian, 2010, Investigating the fidelity of Mg/Ca and other elemental data from reductively cleaned planktonic foraminifera, Paleoceanography, 25, 10.1029/2009PA001796 · DOI
  8. Blaauw, 2011, Flexible paleoclimate age-depth models using an autoregressive gamma process, Bayesian Anal., 6, 457, 10.1214/ba/1339616472 · DOI
  9. Blockley, 2012, Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended INTIMATE1 event stratigraphy to 48,000 b2k, Quat. Sci. Rev., 36, 2, 10.1016/j.quascirev.2011.09.017 · DOI
  10. Boyle, 1985, Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: Changes in deep ocean circulation and chemical inventories, Earth Planet. Sci. Lett., 76, 135, 10.1016/0012-821X(85)90154-2 · DOI
  11. Brennan, 2013, Impact of sea ice variability on the oxygen isotope content of seawater under glacial and interglacial conditions, Paleoceanography, 28, 388, 10.1002/palo.20036 · DOI
  12. Cannariato, 1999, Climatically related millennial-scale fluctuations in strength of California margin oxygen-minimum zone during the past 60 k.y, Geology, 27, 975, 10.1130/0091-7613(1999)027<0975:CRMSFI>2.3.CO;2 · DOI · Paper page
  13. Chang, 2008, Late Quaternary paleoproductivity history on the Vancouver Island margin, western Canada: A multiproxy geochemical study, Can. J. Earth Sci., 45, 1283, 10.1139/E08-038 · DOI
  14. Chang, 2014, Effects of productivity, glaciation and ventilation on late Quaternary sedimentary redox and trace element accumulation on the Vancouver Island margin, western Canada, Paleoceanography, 29, 10.1002/2013PA002581 · DOI
  15. Chappell, 1986, Oxygen isotopes and sea level, Nature, 324, 137, 10.1038/324137a0 · DOI
  16. Chelton, 1982, Monthly mean sea-level variability along the west coast of North America, J. Phys. Oceanogr., 12, 757, 10.1175/1520-0485(1982)012<0757:MMSLVA>2.0.CO;2 · DOI
  17. Chen, 2010, Dynamic millennial-scale climate changes in the northwestern Pacific over the past 40,000 years, Geophys. Res. Lett., 37, 10.1029/2010GL045202 · DOI
  18. COHMAP Members, 1988, Climatic changes of the last 18,000 years: Observations and model simulations, Science, 241, 1043, 10.1126/science.241.4869.1043 · DOI · Paper page
  19. Connolly, 2014, Coastal trapped waves, alongshore pressure gradients, and the California undercurrent*, J. Phys. Oceanogr., 44, 319, 10.1175/JPO-D-13-095.1 · DOI
  20. Cosma, 2008, Chronological constraints on Cordilleran Ice Sheet glaciomarine sedimentation from core MD02-2496 off Vancouver Island (western Canada), Quat. Sci. Rev., 27, 941, 10.1016/j.quascirev.2008.01.013 · DOI
  21. Cummins, 2014, Climatic variability and trends in the surface waters of coastal British Columbia, Prog. Oceanogr., 120, 279, 10.1016/j.pocean.2013.10.002 · DOI
  22. Cummins, 2007, Variability of the North Pacific Current and its bifurcation, Prog. Oceanogr., 75, 253, 10.1016/j.pocean.2007.08.006 · DOI
  23. Davies, 2011, The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia, Paleoceanography, 26, 10.1029/2010PA002051 · DOI · Paper page
  24. Denton, 2010, The last glacial termination, Science, 328, 1652, 10.1126/science.1184119 · DOI
  25. Deplazes, 2013, Links between tropical rainfall and North Atlantic climate during the last glacial period, Nat. Geosci., 6, 213, 10.1038/ngeo1712 · DOI
  26. Douglass, 2006, Interannual variability in northeast Pacific circulation, J. Geophys. Res., 111, 10.1029/2005JC003015 · DOI
  27. Elderfield, 2000, Past temperature and δ18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios, Nature, 405, 442, 10.1038/35013033 · DOI
  28. Flament, 2002, A state variable for characterizing water masses and their diffusive stability: Spiciness, Prog. Oceanogr., 54, 493, 10.1016/S0079-6611(02)00065-4 · DOI
  29. Foreman, 2008, Modeling the generation of the Juan de Fuca Eddy, J. Geophys. Res., 113, 10.1029/2006JC004082 · DOI
  30. Freeland, 2003, Cold halocline in the northern California Current: An invasion of subarctic water, Geophys. Res. Lett., 30, 10.1029/2002GL016663 · DOI
  31. Freeland, 2006, What proportion of the North Pacific Current finds its way into the Gulf of Alaska?, Atmos. Ocean, 44, 321, 10.3137/ao.440401 · DOI
  32. Galbraith, 2008, Consistent relationship between global climate and surface nitrate utilization in the western subarctic Pacific throughout the last 500 ka, Paleoceanography, 23, 10.1029/2007PA001518 · DOI
  33. Gibbons, 2014, Deglacial δ18O and hydrologic variability in the tropical Pacific and Indian Oceans, Earth Planet. Sci. Lett., 387, 240, 10.1016/j.epsl.2013.11.032 · DOI
  34. Harada, 2008, Freshwater impacts recorded in tetraunsaturated alkenones and alkenone sea surface temperatures from the Okhotsk Sea across millennial-scale cycles, Paleoceanography, 23, 10.1029/2006PA001410 · DOI
  35. Hendy, 2010, The paleoclimatic response of the Southern Californian Margin to the rapid climate change of the last 60 ka: A regional overview, Quat. Int., 215, 62, 10.1016/j.quaint.2009.06.009 · DOI
  36. Hendy, 2008, Vulnerability of the Cordilleran Ice Sheet to iceberg calving during late Quaternary rapid climate change events, Paleoceanography, 23, 10.1029/2008PA001606 · DOI · Paper page
  37. Hendy, 2000, Dansgaard-Oeschger Cycles and the California Current System: Planktonic foraminiferal response to rapid climate change in Santa Barbara Basin, Ocean Drilling Program Hole 893A, Paleoceanography, 15, 30, 10.1029/1999PA000413 · DOI
  38. Hendy, 2003, Tropical forcing of North Pacific intermediate water distribution during Late Quaternary rapid climate change?, Quat. Sci. Rev., 22, 673, 10.1016/S0277-3791(02)00186-5 · DOI
  39. Hendy, 2005, Is pore water oxygen content decoupled from productivity on the California Margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia slope, California, Paleoceanography, 20, 10.1029/2004PA001123 · DOI
  40. Hendy, 2002, Apparent synchroneity of submillennial scale climate events between Greenland and Santa Barbara Basin, California from 30-10 ka, Quat. Sci. Rev., 21, 1167, 10.1016/S0277-3791(01)00138-X · DOI
  41. Hendy, 2004, Intermittent existence of a southern Californian upwelling cell during submillennial climate change of the last 60 kyr, Paleoceanography, 19, 10.1029/2003PA000965 · DOI
  42. Hickey, 2008, Why is the northern end of the California Current system so productive?, Oceanography, 21, 90, 10.5670/oceanog.2008.07 · DOI
  43. Jonkers, 2013, Seasonal Mg/Ca variability of N. pachyderma (s) and G. bulloides: Implications for seawater temperature reconstruction, Earth Planet. Sci. Lett., 376, 137, 10.1016/j.epsl.2013.06.019 · DOI
  44. Justino, 2005, Synoptic reorganization of atmospheric flow during the last glacial maximum, J. Clim., 18, 2826, 10.1175/JCLI3403.1 · DOI
  45. Keigwin, 1989, Late Quaternary paleochemistry of high-latitude surface waters, Palaeogeogr. Palaeoclimatol. Palaeoecol., 73, 85, 10.1016/0031-0182(89)90047-3 · DOI
  46. Kennett, 2000, Latest Quaternary paleoclimatic and radiocarbon chronology, Hole 1017E, Southern California margin, Proc. Ocean Drill. Program Sci. Results, 167, 249
  47. Kienast, 2001, Sea surface temperatures in the subarctic northeast Pacific reflect millennial-scale climate oscillations during the last 16 kyrs, Geophys. Res. Lett., 28, 1563, 10.1029/2000GL012543 · DOI
  48. Kienast, 2002, Nitrogen isotope and productivity variations along the northeast Pacific margin over the last 120 kyr: Surface and subsurface paleoceanography, Paleoceanography, 17, 7-1, 10.1029/2001PA000650 · DOI
  49. Kuroyanagi, 2004, Vertical distribution of living planktonic foraminifera in the seas around Japan, Mar. Micropaleontol., 53, 173, 10.1016/j.marmicro.2004.06.001 · DOI
  50. Leduc, 2009, ITCZ rather than ENSO signature for abrupt climate changes across the tropical Pacific?, Quat. Res., 72, 123, 10.1016/j.yqres.2009.03.006 · DOI
  51. Leduc, 2010, Changes in Eastern Pacific ocean ventilation at intermediate depth over the last 150 kyr BP, Earth Planet. Sci. Lett., 298, 217, 10.1016/j.epsl.2010.08.002 · DOI
  52. LeGrande, 2006, Global gridded data set of the oxygen isotopic composition in seawater, Geophys. Res. Lett., 33, 10.1029/2006GL026011 · DOI · Paper page
  53. Locarnini, 2006, World Ocean Atlas 2005, Volume 1: Temperature, 182
  54. Liu, 1989, The eastern tropical Pacific as a source of 15N-enriched nitrate in seawater off southern California, Limnol. Oceanogr., 34, 820, 10.4319/lo.1989.34.5.0820 · DOI
  55. Lynn, 1987, The California Current system: The seasonal variability of its physical characteristics, J. Geophys. Res., 92, 12,947, 10.1029/JC092iC12p12947 · DOI · Paper page
  56. Manabe, 1988, Two stable equilibria of a coupled ocean-atmosphere model, J. Clim., 1, 841, 10.1175/1520-0442(1988)001<0841:TSEOAC>2.0.CO;2 · DOI
  57. Martin, 2002, A simple evaluation of cleaning procedures on fossil benthic foraminiferal Mg/Ca, Geochem. Geophys. Geosyst., 3, 10.1029/2001GC000280 · DOI
  58. Masson, 1999, Numerical simulations of a buoyancy-driven coastal countercurrent off Vancouver Island, J. Phys. Oceanogr., 29, 418, 10.1175/1520-0485(1999)029<0418:NSOABD>2.0.CO;2 · DOI
  59. Masson, 2012, Modeling seasonal to interannual ocean variability of coastal British Columbia, J. Geophys. Res., 117, 10.1029/2012JC008151 · DOI
  60. Max, 2012, Sea surface temperature variability and sea-ice extent in the subarctic northwest Pacific during the past 15,000 years, Paleoceanography, 27, 10.1029/2012PA002292 · DOI
  61. Meinvielle, 2013, Decadal water-property trends in the California Undercurrent, with implications for ocean acidification, J. Geophys. Res. Oceans, 118, 6687, 10.1002/2013JC009299 · DOI
  62. Mix, 1999, Mechanisms of Global Climate Change at Millennial Time Scales, 127, 10.1029/GM112p0127 · DOI
  63. Mosher, 2004, Late Quaternary deglaciation and sea-level history of eastern Juan de Fuca Strait, Cascadia, Quat. Int., 121, 23, 10.1016/j.quaint.2004.01.021 · DOI
  64. North Greenland Ice Core Project members (NGRIP), 2004, High-resolution record of Northern Hemisphere climate extending into the last interglacial period, Nature, 431, 147, 10.1038/nature02805 · DOI
  65. Ohkushi, 2013, Quantified intermediate water oxygenation history of the NE Pacific: A new benthic foraminiferal record from Santa Barbara basin, Paleoceanography, 28, 453, 10.1002/palo.20043 · DOI
  66. Okumura, 2009, North Pacific climate response to freshwater forcing in the subarctic North Atlantic: Oceanic and atmospheric pathways, J. Clim., 22, 1424, 10.1175/2008JCLI2511.1 · DOI
  67. Pak, 2004, Seasonal and interannual variation in Santa Barbara Basin water temperatures observed in sediment trap foraminiferal Mg/Ca, Geochem. Geophys. Geosyst., 5, 10.1029/2004GC000760 · DOI
  68. Pak, 2012, Millennial scale changes in sea surface temperature and ocean circulation in the northeast Pacific, 10-60 kyr BP, Paleoceanography, 27, 10.1029/2011PA002238 · DOI
  69. Pausata, 2011, The key role of topography in altering North Atlantic atmospheric circulation during the last glacial period, Clim. Past, 7, 1089, 10.5194/cp-7-1089-2011 · DOI
  70. Praetorius, 2014, Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming, Science, 345, 444, 10.1126/science.1252000 · DOI
  71. Reimer, 2013, INTCAL13 and MARINE13 radiocarbon age calibration curves 0-50,000 years cal BP, Radiocarbon, 55, 1869, 10.2458/azu_js_rc.55.16947 · DOI · Paper page
  72. Reynolds, 1986, Seasonal production and morphologic variation of Neogloboquadrina pachyderma (Ehrenberg) in the Northeast Pacific, Micropaleontology, 32, 1, 10.2307/1485696 · DOI
  73. Riethdorf, 2013, Deglacial development of (sub) sea surface temperature and salinity in the subarctic northwest Pacific: Implications for upper-ocean stratification, Paleoceanography, 28, 91, 10.1002/palo.20014 · DOI
  74. Robinson, 1981, Radiocarbon corrections for marine shell dates with application to southern Pacific Northwest coast prehistory, Syesis, 14, 45
  75. Sautter, 1989, Seasonal succession of planktonic foraminifera: Results from a four-year time-series sediment trap experiment in the northeast Pacific, J. Foraminiferal Res., 19, 253, 10.2113/gsjfr.19.4.253 · DOI
  76. Schrag, 1996, Pore fluid constraints on the temperature and oxygen isotopic composition of the glacial ocean, Science, 272, 1930, 10.1126/science.272.5270.1930 · DOI
  77. Seki, 2002, Millennial climate oscillations in NE Pacific surface waters over the last 82 kyr: New evidence from alkenones, Geophys. Res. Lett., 29, 10.1029/2002GL015200 · DOI
  78. Shackleton, 1974, Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus, Colloq. Int. C.N.R.S., 219, 203
  79. Strub, 2002, Altimeter-derived surface circulation in the large-scale NE Pacific Gyres. Part 1. Seasonal variability, Prog. Oceanogr., 53, 163, 10.1016/S0079-6611(02)00029-0 · DOI
  80. Sydeman, 2011, Does positioning of the North Pacific Current affect downstream ecosystem productivity?, Geophys. Res. Lett., 38, 10.1029/2011GL047212 · DOI
  81. Taylor, 2014, Deglacial ocean warming and marine margin retreat of the Cordilleran Ice Sheet in the North Pacific Ocean, Earth Planet. Sci. Lett., 403, 89, 10.1016/j.epsl.2014.06.026 · DOI
  82. Thomson, 2010, Poleward reach of the California Undercurrent extension, J. Geophys. Res., 115, 10.1029/2010JC006280 · DOI
  83. Timmermann, 2004, Surface temperature control in the North and tropical Pacific during the last glacial maximum, Clim. Dyn., 23, 10.1007/s00382-004-0434-9 · DOI
  84. Waelbroeck, 2002, Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records, Quat. Sci. Rev., 21, 295, 10.1016/S0277-3791(01)00101-9 · DOI
  85. Zhang, 2005, Simulated tropical response to a substantial weakening of the Atlantic thermohaline circulation, J. Clim., 18, 1853, 10.1175/JCLI3460.1 · DOI

Cited by

Sorted by citations

Metadata

Authors
Taylor, M. A., Hendy, I. L., & Pak, D. K.
Affiliations
  • Department of Earth and Environmental Sciences; University of Michigan; Ann Arbor Michigan USA
  • Marine Science Institute; University of California; Santa Barbara California USA
Venue
Paleoceanography
Publisher
American Geophysical Union (AGU)
Published
2015-09
Volume
30
Issue
9
Pages
1168-1182
ISSN
0883-8305
DOI
10.1002/2014pa002738
Cited by
13
References
1
Language
en
Licence
Funders
  • Research Fund (UO38916)
  • Rackham Graduate Student Research (UO35598)
  • Scott Turner through the University of Michigan

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