Lang, David C; Bailey, Ian; Wilson, Paul A; Chalk, Thomas B; Foster, Gavin L; Gutjahr, Marcus (2016): Estimates of %NCW bathing deep North Atlantic (IODP Site 306-U1313) over the past ~3.3 Ma. PANGAEA, https://doi.org/10.1594/PANGAEA.860974, Supplement to: Lang, DC et al. (2016): Incursions of southern-sourced water into the deep North Atlantic during late Pliocene glacial intensification. Nature Geoscience, 9(5), 375-379, https://doi.org/10.1038/ngeo2688
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The circulation and internal structure of the oceans exert a strong influence on Earth's climate because they control latitudinal heat transport and the segregation of carbon between the atmosphere and the abyss (Sigman et al., 2010, doi:10.1038/nature09149). Circulation change, particularly in the Atlantic Ocean, is widely suggested (Bartoli et al., 2005, doi:10.1016/j.epsl.2005.06.020; Haug and Tiedemann, 1998, doi:10.1038/31447; Woodard et al., 2014, doi:10.1126/science.1255586; McKay et al., 2012, doi:10.1073/pnas.1112248109) to have been instrumental in the intensification of Northern Hemisphere glaciation when large ice sheets first developed on North America and Eurasia during the late Pliocene, approximately 2.7 million years ago (Bailey et al., 2013, doi:10.1016/j.quascirev.2013.06.004). Yet the mechanistic link and cause/effect relationship between ocean circulation and glaciation are debated. Here we present new records of North Atlantic Ocean structure using the carbon and neodymium isotopic composition of marine sediments recording deep water for both the Last Glacial to Holocene (35-5 thousand years ago) and the late Pliocene to earliest Pleistocene (3.3-2.4 million years ago). Our data show no secular change. Instead we document major southern-sourced water incursions into the deep North Atlantic during prominent glacials from 2.7 million years ago. Our results suggest that Atlantic circulation acts as a positive feedback rather than as an underlying cause of late Pliocene Northern Hemisphere glaciation. We propose that, once surface Southern Ocean stratification (Sigman, et al., 2004, doi:10.1038/nature02357) and/or extensive sea-ice cover (McKay et al., 2012, doi:10.1073/pnas.1112248109) was established, cold-stage expansions of southern-sourced water such as those documented here enhanced carbon dioxide storage in the deep ocean, helping to increase the amplitude of glacial cycles.
Median Latitude: 41.000012 * Median Longitude: -32.957159 * South-bound Latitude: 41.000000 * West-bound Longitude: -32.957310 * North-bound Latitude: 41.000023 * East-bound Longitude: -32.957010
Date/Time Start: 2004-03-28T00:00:00 * Date/Time End: 2004-04-02T00:00:00
Estimates (and their 95% confidence intervals) of the precentage of northern component water (%NCW) bathing the deep North Atlantic (at IODP Site U1313, ~3400 m water depth) during: (1) the late Pliocene and earliest Pleistocene intensification of northern hemisphere glaciation, ~2.4 to 3.3 Ma (derived from the Nd isotope composition of fish debris; shown in Figure 2h of Lang et al., 2016) and ~0.013 to 3.3 Ma (derived from the carbon isotope composition of epibenthic foraminiferal calcite; shown in Figure 1b in Lang et al., 2016). See Lang et al. (2016) for the exact methods.
Datasets listed in this publication series
- Lang, DC; Bailey, I; Wilson, PA et al. (2016): Detrital carbonate, volcanics and IRD counts of IODP Site 306-U1313C. https://doi.org/10.1594/PANGAEA.860986
- Lang, DC; Bailey, I; Wilson, PA et al. (2016): Estimates of Northern Component Water based on Nd-isotopes of IODP Site 306-U1313. https://doi.org/10.1594/PANGAEA.860972
- Lang, DC; Bailey, I; Wilson, PA et al. (2016): Estimates of Northern Component Water based on benthic foraminifera δ¹³C measurement of IODP Site 306-U1313. https://doi.org/10.1594/PANGAEA.860973
- Lang, DC; Bailey, I; Wilson, PA et al. (2016): Nd-isotope of fish debris and Fe-Mn-leached sediments of IODP Site 306-U1313. https://doi.org/10.1594/PANGAEA.860987
- Lang, DC; Bailey, I; Wilson, PA et al. (2016): Nd-isotope of last glacial to Holocene sediments of IODP Site 306-U1313. https://doi.org/10.1594/PANGAEA.860985