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Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint
Open accessAbstract
Millennial climate oscillations of the glacial interval are interrupted by extreme events, the so‐called Heinrich events of the North Atlantic. Their near‐global footprint is a testament to coherent interactions among Earth's atmosphere, oceans, and cryosphere on millennial timescales. Heinrich detritus appears to have been derived from the region around Hudson Strait. It was deposited over approximately 500 ± 250 years. Several mechanisms have been proposed for the origin of the layers: binge‐purge cycle of the Laurentide ice sheet, jökulhlaup activity from a Hudson Bay lake, and an ice shelf buildup/collapse fed by Hudson Strait. To determine the origin of the Heinrich events, I recommend (1) further studies of the timing and duration of the events, (2) further sedimentology study near the Hudson Strait, and (3) greater spatial and temporal resolution studies of the layers as well as their precursory intervals. Studies of previous glacial intervals may also provide important constraints.
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Cites
Sea-level fluctuations during the last glacial cycle
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Trajectories of the Earth System in the Anthropocene
Steffen, W., Rockström, J., Richardson, K., Lenton, T. M., Folke, C., Liverman, D., Summerhayes, C. P., Barnosky, A. D., Cornell, S. E., Crucifix, M., et al. (2018) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1810141115 · Cited by 3,139
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
Lambeck, K., Rouby, H., Purcell, A., Sun, Y., & Sambridge, M. (2014) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1411762111 · Cited by 2,215
Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation
Carlson, A. E., & Clark, P. U. (2012) · Reviews of Geophysics · doi:10.1029/2011rg000371 · Cited by 249
Dalton, A. S., Stokes, C. R., & Batchelor, C. L. (2022) · Earth-Science Reviews · doi:10.1016/j.earscirev.2021.103875 · Cited by 104
Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography
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A mechanism for reconciling the synchronisation of Heinrich events and Dansgaard-Oeschger cycles
Schannwell, C., Mikolajewicz, U., Kapsch, M.-L., & Ziemen, F. (2024) · Nature Communications · doi:10.1038/s41467-024-47141-7 · Cited by 6
Metadata
- Authors
- Hemming, S. R.
- Venue
- Reviews of Geophysics
- Publisher
- American Geophysical Union (AGU)
- Published
- 2004-03
- Volume
- 42
- Issue
- 1
- ISSN
- 0096-1043 (ISSN-L)
- 8755-1209
- 1944-9208
- OpenAlex
- W2051126029
- Cited by
- 1,526
- References
- 2
- FWCI
- 32.86
- Type
- journal article
- Language
- en
- Open access
- bronze
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