Changes in surface salinity of the North Atlantic Ocean during the last deglaciation

• Published in: Nature (London) 1992-08, Vol.358 (6386), p.485-488
• Main Authors: Duplessy, J. C, Labeyrie, L, Arnold, M, Paterne, M, Duprat, J, van Weering, T. C. E
• Format: Article
• Language: English
• Subjects: Advection; Climate; Climate change; Continental interfaces, environment; Deglaciation; Earth sciences; Earth, ocean, space; Evaporation; Exact sciences and technology; Humanities and Social Sciences; Hydrologic cycle; Injection; Latitude; letter; Marine; Marine and continental quaternary; Meltwater; multidisciplinary; Ocean, Atmosphere; Oceanography; Oceans; Paleontology; Salinity; Science; Science (multidisciplinary); Sciences of the Universe; Sea surface temperature; Surface water; Surficial geology; Temperature; Thermohaline circulation
• ISSN: 0028-0836; 1476-4687
• DOI: 10.1038/358485a0

ABRUPT and short climate changes, such as the Younger Dryas, punctuated the last glacial-to-interglacial transition 1–4 . Broecker et al. 5 proposed that these may have been caused by an interruption of thermohaline circulation as inputs of glacial meltwater freshened the surface waters of the North Atlantic. The finding 6 that meltwater discharge was minimal during the Younger Dryas, however, led to the suggestion that the surface-water salinity drop might have been caused instead by changes in the freshwater budget (the difference between precipitation and evaporation), accompanied by a reduction in poleward advection of saline subtropical water. Here we use micropalaeontological and stable-isotope records from foraminifera in two cores from the North Atlantic to generate two continuous, high-resolution records of sea surface temperature and salinity changes over the past 18,000 years. Despite the injection of glacial meltwater during warm episodes, we find that sea surface salinity and temperature remain positively correlated during deglaciation. Cold, low-salinity events occurred during the early stages of deglaciation (14,500–13,000 years ago) and the Younger Dryas, but the minor injections of meltwater at high latitudes during these events are insufficient to account for the observed salinity changes. We conclude that an additional feedback from changes in the hydrological cycle and in advection was necessary to trigger changes in thermohaline circulation and thus in climate. This feedback did not act when the meltwater injection occurred at low latitude.