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Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland

Nature volume 397, pages 515–517 (1999)Cite this article

Abstract

Climate fluctuations during the past millennium are relatively well documented1. On a longer timescale, there is growing evidence of millennial-scale variability of Holocene climate, at periodicities of ∼2,500 and 950 years (possibly caused by changes in solar flux)2,3 and ∼1,500 years (maybe related to an internal oscillation of the climate system)4,5,6. But the involvement of deep water masses in these Holocene climate changes has yet to be established. Here we use sediment grain-size data from the Iceland basin to reconstruct past changes in the speed of deep-water flow. The study site is under the influence of Iceland–Scotland Overflow Water (ISOW), the flow of which is an important component of the ‘thermohaline’ circulation that modulates European climate. Flow changes coincide with some known climate events (the Little Ice Age and the Mediaeval Warm Period), and extend over the entire Holocene epoch with aquasi-periodicity of ∼1,500 years. The grain-size data indicate afaster ISOW flow when the climate of northern Europe is warmer. However, a second mode of operation is observed in the early Holocene, when warm climate intervals are associated with slower ISOW flow. At that time the melting remnant of land-based, glacial-age ice may have provided a sufficient source of fresh water to the ocean to reduce ISOW flow south of Iceland.

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Figure 1: Data from kasten core NEAP-15K with an inset map showing its location in the south Iceland basin and the simplified regional flow of ISOW.
Figure 2: North Atlantic Holocene palaeoenvironmental proxy records on a calendar years BP(and AD/BC) basis.
Figure 3: Spectral analysis by the Blackman-Tukey technique34 of the sortable silt mean size record from NEAP-15K using data as shown in Fig. 2b.

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Acknowledgements

We thank S. Crowhurst for help in the spectral analysis of the data presented here, N.Shackleton for comments on an earlier draft, and R. Dickson for hydrographic observations. This work was supported by UK NERC for the North East Atlantic Palaeoceanography and Climate Change project (NEAPACC).

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  1. Department of Earth Sciences, University of Cambridge, Downing Street, CB2 3EQ, Cambridge, UK

    Giancarlo G. Bianchi & I. Nicholas McCave

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  1. Giancarlo G. Bianchi
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Bianchi, G., McCave, I. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature 397, 515–517 (1999). https://doi.org/10.1038/17362

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