The DOI matches its Crossref record; 31 of the 31 references it cites were found in a registry or an index.
Pliocene‐Pleistocene ice rafting history and cyclicity in the Nordic Seas during the last 3.5 Myr
Abstract
A continuous 3.5 Myr IRD record was produced from Ocean Drilling Program (ODP) Site 907. A timescale based on magnetic polarity chrons, oxygen isotope stratigraphy (for the last 1Myr) and orbital tuning was developed. The record documents a stepwise inception of large‐scale glacial cycles in the Nordic Seas region, the first being a marked expansion of the Greenland ice sheet at 3.3 Ma. A second step occurred at 2.74 Ma by an expansion of large scale ice sheets in the Northern Hemisphere. Ice sheet variability around the Nordic Seas was tightly coupled to global ice volume over the past 3.3 Myr. Between 3 and 1 Ma, most of the variance of the IRD signal is in the 41 kyr band, whereas the last 1 Myr is characterized by stronger 100 kyr variance. The Gamma Ray Porosity Evaluator (GRAPE) density record is closely linked with IRD variations and documents sub orbital variability resembling the late Quaternary Heinrich/Bond cycles.
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.
Integrity signals
Registry
Cites
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.
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
Insolation values for the climate of the last 10 million years
Berger, A., & Loutre, M. F. (1991) · Quaternary Science Reviews · doi:10.1016/0277-3791(91)90033-q · Cited by 4,386
Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic
Cande, S. C., & Kent, D. V. (1995) · Journal of Geophysical Research: Solid Earth · doi:10.1029/94jb03098 · Cited by 3,730
Evolution of indirect reciprocity by image scoring
Nowak, M. A., & Sigmund, K. (1998) · Nature · doi:10.1038/31225 · Cited by 2,700
Tectonic forcing of late cenozoic climate.
Raymo, M. E., & Ruddiman, W. F. (1992) · Nature · doi:10.1038/359117a0 · Cited by 2,341
Correlations between climate records from North Atlantic sediments and Greenland ice
Bond, G., Broecker, W., Johnsen, S., McManus, J., Labeyrie, L., Jouzel, J., & Bonani, G. (1993) · Nature · doi:10.1038/365143a0 · Cited by 2,333
Macintosh Program performs time‐series analysis
Paillard, D., Labeyrie, L., & Yiou, P. (1996) · Eos, Transactions American Geophysical Union · doi:10.1029/96eo00259 · Cited by 2,074
Milankovitch and Climate: Understanding the Response to Astronomical Forcing
(1984) · Springer eBooks · doi:10.1007/978-94-017-4841-4 · Cited by 1,890
An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677
Shackleton, N. J., Berger, A., & Peltier, W. R. (1990) · Transactions of the Royal Society of Edinburgh: Earth Sciences · doi:10.1017/s0263593300020782 · Cited by 1,631
Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation
Haug, G. H., & Tiedemann, R. (1998) · Nature · doi:10.1038/31447 · Cited by 977
Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic Ocean
Ruddiman, W. F., Raymo, M. E., Martinson, D. G., Clement, B. M., & Backman, J. (1989) · Paleoceanography · doi:10.1029/pa004i004p00353 · Cited by 844
Cited by
Atmospheric CO2 decline during the Pliocene intensification of Northern Hemisphere glaciations
Bartoli, G., Hönisch, B., & Zeebe, R. E. (2011) · Paleoceanography · doi:10.1029/2010pa002055 · Cited by 309
Krause, J., Unger, T., Noçon, A., Malaspinas, A.-S., Kolokotronis, S.-O., Stiller, M., Soibelzon, L., Spriggs, H., Dear, P. H., Briggs, A. W., et al. (2008) · BMC Evolutionary Biology · doi:10.1186/1471-2148-8-220 · Cited by 284
Metadata
- Authors
- Jansen, E., Fronval, T., Rack, F., & Channell, J. E. T.
- Venue
- Paleoceanography
- Publisher
- American Geophysical Union (AGU)
- Published
- 2000-12
- Volume
- 15
- Issue
- 6
- Pages
- 709-721
- ISSN
- 0883-8305 (ISSN-L)
- 1944-9186
- OpenAlex
- W1992590047
- Cited by
- 254
- References
- 31
- FWCI
- 4.29
- Type
- journal article
- Language
- en
- Open access
- closed
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
How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Pliocene‐Pleistocene ice rafting history and cyclicity in the Nordic Seas during the last 3.5 Myr. https://app.cochat.ai/papers/10.1029/1999pa000435
- The paper
- Jansen, E., Fronval, T., Rack, F., & Channell, J. E. T. (2000). Pliocene‐Pleistocene ice rafting history and cyclicity in the Nordic Seas during the last 3.5 Myr. Paleoceanography. https://doi.org/10.1029/1999pa000435
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.