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Nitrate flux into the euphotic zone near Bermuda

Abstract

Throughout most of the year, there exists within the North Atlantic subtropical ocean mixed layer a3He excess which can only be attributed to a flux of tritiugenic3He from below. The upward flux required to support this excess can be computed as the convolution of the time series of3He excess and gas-exchange rate. This flux is quantitatively consistent with the long-term evolution of the main thermocline inventories of tritium and 3He. Using the observed correlation of 3He with nitrate within the upper main thermocline, I estimate the annually averaged upward flux of nitrate into the euphotic zone to be 0.6 ±0.2 moles m−2 per yr. This flux is sufficient to support a new, non-regenerative primary productivity in excess of 3 moles carbon m−2per yr.

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Jenkins, W. Nitrate flux into the euphotic zone near Bermuda. Nature 331, 521–523 (1988). https://doi.org/10.1038/331521a0

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