The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.
North Atlantic circulation and reservoir age changes over the past 41,000 years
Abstract
Constraints on the timing of Atlantic meridional overturning circulation (AMOC) changes during the last deglaciation are fundamental to understanding the climate's rapid response to insolation forcing. However, uncertainty about high‐latitude North Atlantic (HLNA) radiocarbon reservoir ages has previously precluded robust age model development for this critical region. HLNA reservoir ages also serve as a proxy for AMOC strength. We present regionally averaged HLNA reservoir ages for 0 to 41 thousand years before the present (kyr BP) based on over 500 radiocarbon dates from 33 North Atlantic cores. An early deglacial increase to >1000 14 C yr reservoir ages between 18.5 and 16.5 kyr BP suggests reduced AMOC before peak Heinrich Stadial 1 (HS1) ice‐rafted debris (IRD). A rapid decrease in reservoir ages coincident with the IRD maximum at 16 kyr BP indicates strong stratification of the upper water column caused by massive freshwater release.
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?
Changes in ocean circulation, such as slowdown of meridional overturning circulation during the last glacial (ca. 55-15 cal kBP), were likely responsible for additional increases in MRA.
“Changes in ocean circulation, such as the slowdown of the meridional overturning circulation during the last glacial (ca. 55 -15 cal kBP) were likely responsible for additional increases in MRA (e.g. Stern and Lisiecki 2013; Skinner et al. 2017).”
From The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) (2020) · cites this paper as Stern and Lisiecki 2013
Citations
Cites
IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey, C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., et al. (2013) · Radiocarbon · doi:10.2458/azu_js_rc.55.16947 · Cited by 14,591
Carbon Isotope Constraints on the Deglacial CO 2 Rise from Ice Cores
Schmitt, J., Schneider, R., Elsig, J., Leuenberger, D., Lourantou, A., Chappellaz, J., Köhler, P., Joos, F., Stocker, T. F., Leuenberger, M., et al. (2012) · Science · doi:10.1126/science.1217161 · Cited by 416
Flagged first, then by citations
Research works printed but not linked: 39
- 10.5194/cp‐7‐1297‐2011 · DOI
- 10.1126/science.1167441 · DOI
- 10.1016/j.quageo.2008.12.002 · DOI
- 10.1016/0012‐821X(94)90112‐0 · DOI · Paper page
- 10.1126/science.289.5483.1321 · DOI
- 10.1126/science.274.5290.1155 · DOI
- 10.1126/science.1123300 · DOI
- 10.1016/j.quascirev.2012.10.015 · DOI
- 10.1016/j.quascirev.2009.07.007 · DOI
- 10.1029/2011RG000371 · DOI · Paper page
- 10.1130/G25080A.1 · DOI
- 10.1029/2004PA001021 · DOI
- 10.1038/nature05301 · DOI
- 10.1016/j.epsl.2005.09.061 · DOI
- 10.1029/2010PA002084 · DOI
- 10.1038/nature11822 · DOI
- 10.1029/2006PA001298 · DOI
- 10.1016/j.quascirev.2009.11.010 · DOI
- 10.1073/pnas.1104772108 · DOI
- 10.1038/nature02494 · DOI
- 10.1029/2007PA001416 · DOI
- 10.1038/nature02805 · DOI
- 10.1130/G30389.1 · DOI
- 10.1126/science.1190612 · DOI
- 10.1016/j.quascirev.2008.07.009 · DOI
- 10.1126/science.1226368 · DOI
- 10.1029/2006GC001321 · DOI
- 10.1016/j.quascirev.2006.04.010 · DOI
- 10.1017/S0033822200034202 · DOI · Paper page
- 10.1016/j.epsl.2008.01.024 · DOI
- 10.1007/s00382‐009‐0578‐8 · DOI
- 10.1038/nature10915 · DOI
- 10.1038/NGEO1026 · DOI
- 10.5194/cp‐4‐47‐2008 · DOI
- 10.1016/j.gloplacha.2010.06.003 · DOI
- 10.1002/jqs.1442 · DOI
- 10.1038/35089060 · DOI
- 10.1029/2010PA002007 · DOI
- 10.1126/science.1064618 · DOI
Cited by
Sorted by citations
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
Reimer, P. J., Austin, W. E. N., Bard, E., Bayliss, A., Blackwell, P. G., Bronk Ramsey, C., Butzin, M., Cheng, H., Edwards, R. L., Friedrich, M., et al. (2020) · Radiocarbon · doi:10.1017/rdc.2020.41 · Cited by 7,900
“Changes in ocean circulation, such as the slowdown of the meridional overturning circulation during the last glacial (ca. 55 – 15 cal kBP) were likely responsible for additional increases in MRA (e.g. Stern and Lisiecki 2013; Skinner et al. 2017).”
BackgroundCentennial-scale changes in the global carbon cycle during the last deglaciation
Marcott, S. A., Bauska, T. K., Buizert, C., Steig, E. J., Rosen, J. L., Cuffey, K. M., Fudge, T. J., Severinghaus, J. P., Ahn, J., Kalk, M. L., et al. (2014) · Nature · doi:10.1038/nature13799 · Cited by 580
Metadata
- Authors
- Stern, J. V., & Lisiecki, L. E.
- Affiliations
- University of California, Santa Barbara (US)
- Corresponding author
- Stern, Joseph V.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2013-07-19
- Volume
- 40
- Issue
- 14
- Pages
- 3693-3697
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W1897950478
- Cited by
- 103
- References
- 2
- Citations by year
- 2026: 5 · 2025: 6 · 2024: 2 · 2023: 6 · 2022: 10 · 2021: 11 · 2020: 8 · 2019: 10 · 2018: 10 · 2017: 9 · 2016: 8 · 2015: 9 · 2014: 9
- FWCI
- 5.64
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geophysical Research Letters (publishedVersion)
- eScholarship (California Digital Library) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
- Keywords
- Atlantic meridional overturning circulation, radiocarbon reservoir age, North Atlantic, last deglaciation, Heinrich Stadial 1, ice-rafted debris, freshwater discharge, age model, insolation forcing, 41 kyr cycle
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
