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Nitrite in a deep oxygenated environment - the Japan/East Sea and Ulleung Basin

Nitrite in a deep oxygenated environment - the Japan/East Sea and Ulleung Basin. L. D. Talley, P. Y. Tishchenko, G. Mitchell G., D.-J. Kang, D.-H. Min, A. Nedashkovskiy, D. Masten, P. Robbins

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Nitrite in a deep oxygenated environment - the Japan/East Sea and Ulleung Basin

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  1. Nitrite in a deep oxygenated environment - the Japan/East Sea and Ulleung Basin L. D. Talley, P. Y. Tishchenko, G. Mitchell G., D.-J. Kang, D.-H. Min, A. Nedashkovskiy, D. Masten, P. Robbins Scripps Institution of Oceanography, Pacific Oceanological Institute, Seoul National University, University of Washington CREAMS ‘01 February, 2001, Honolulu, HI Vertical sections from summer 1999 Revelle and Khromov and winter Khromov survey are on the web: http://sam.ucsd.edu/onr_data

  2. Nitrite Nitrite is an intermediate product of nitrate reduction or ammonium oxidation. Lifetime: 3 to 30 days - presence indicates active biological process. Nitrite is created by *(1) oxidation of ammonium by nitrifying bacteria (2) reduction of nitrate by phytoplankton (euphotic zone) *(3) reduction of nitrate by denitrifying bacteria Nitrite is removed by (1) utilization by phytoplankton (euphotic zone) (2) bacterial oxidation to nitrate (3) bacterial reduction (denitrification process)

  3. Usual nitrite occurrence 1. Euphotic zone: primary nitrite maximum (PNM) at the base of the euphotic zone, coincident with a nitracline (high nitrate gradient). Created mainly by oxidation of ammonium, plus some phytoplankton reduction, and limited phytoplankton uptake due to light limitation. Found throughout ocean, easily distinguished in Japan/East Sea 2. Nearly anoxic regions, mainly in the eastern tropical regions, such as in the Pacific. Created by reduction of nitrate by denitrifying bacteria, part of process to complete denitrification (to N2). 3. Occurrence near sediments not so often described.

  4. Sediment processes affecting nitrogen; NW Pacific oxic waters Water column in Japan, Okhotsk and Bering Seas is full of oxygen, so subeuphotic zone nitrite cannot be due to denitrification in the water column. Sediment processes: possibly coupled denitrification and nitrification as suggested by a number of authors. Large-scale effect is of denitrification. Existence of deep nitrite (in turbid bottom boundary layer): sediment-water interface is wide. Nitrification (oxidation) could occur in upper interface, producing NO2, using ammonium from decay of organic matter. Denitrification (reduction) farther down, net downward flux of NO3 out of water column and into sediments.

  5. Summer 99 and winter 2000

  6. Southernmost Ulleung Basin section: nitrite at bottom

  7. Ulleung Basin, southernmost section Nitrite Nitrate

  8. All profiles of nitrite in the Ulleung Basin The 0.01 “noise” is the bottom sample on many stations. It coincides with turbid layer, lowered oxygen, lowered nitrate, lowered alkalinity.

  9. Ulleung Basin: profiles at station 10 (1400 m deep, southern section). Bottom boundary layer: nitrite enhancement, O2 depletion, NO3 depletion, N* suggesting denitrification, high turbidity (water full of sediment) NO2 NO3 O2 Overhead showing light transmission: turbid bottom boundary layer N* PO4

  10. Location of measurable bottom nitrite “Measurable” is > 0.004 mol/kg (rounded to 0.01 in these files). Using standard autoanalyzer, colorimetric procedure (Scripps Institution of Oceanography Oceanographic Data Facility). (Much smaller quantities are measured with other specialized techniques.) Next overheads: location of bottom nitrite and depth ranges. Showing that the Ulleung Basin in particular has measurable bottom nitrite but not in the middle at the deepest stations. Also the Primorye and Honshu coasts (to 500 or 1000 m) Extension: look at Okhotsk and Bering Sea nitrite as well.

  11. Bottom nitrite and oxygen

  12. Sediment composition Overheads showing: 1) high percentage of organic carbon in the sediments in the Ulleung Basin and around the margins - coinciding with occurrence of deep nitrite. High percentages are similar to (greater than) percentages found in Washington coast sediment measurements that showed denitrification (Devol, 1991) 2) schematic of bottom composition near Hokkaido, showing fissures, gas hydrates that mix bottom sediments. (Takeuchi et al., 1998) 3) strong currents and eddies extending to bottom might also result in turbidity, extending the sediment processes up into the water column.

  13. Larger-scale effects of sediment denitrification? Denitrification can be recognized using N* (Gruber and Sarmiento, 1997): based on N:P ratio for nitrification and denitrification. Values greater than zero indicate nitrogen fixation. Values less than zero indicate denitrification. Consider N* and the N:P ratio in the Japan/East, Okhotsk and Bering Seas, as well as in the Pacific.

  14. N:P ratio and the 1:16 ratio line. Excursion left of line -> denitrification; right of line -> N fixation. PO4 Japan/East Sea Okhotsk Sea Bering Sea Tsushima Strait

  15. Denitrification in Okhotsk Sea is most pronounced. Denitrification in Japan/East Sea below the shallow pycnocline Sigma 0 Depth N* Japan/East Sea, Okhotsk Sea, Bering Sea Tsushima Strait N*

  16. Pacific-wide N* distribution Overhead shows N* for the Pacific WOCE sections (Robbins). Low N* in 2 regions: eastern tropical Pacific (nearly anoxic water column -> denitrification) and NW Pacific (apparently denitrification in the sediments) NW Pacific has just P14N and P01W in the Bering and Okhotsk Seas. Additional Okhotsk Sea survey, already shown, highlights denitrification effects in Okhotsk Sea in comparison with Bering, which is weaker, but which is often referred to because of Geosecs data.

  17. Mid-depth oxygen minimum: is there a link to sedimentary processes? Ulleung Basin, Yamato Rise, Japan Basin Primorye, Hokkaido

  18. Monotonic decrease in oxygen of East Sea Proper Water, as noted by many others. Could O2 utilization be higher than usually assumed for open ocean conditions, due to enhanced sedimentary processes? The decrease in deep oxygen does not necessarily mean that there is no deep water formation, only that it is formed at a lower rate now than prior to 1930s. (note that we observed penetration last, warm winter to >1000m both on slope and in convection patch, maybe bottom) Vertical oxygen profiles from the central Japan Basin. From Kim et al. (1998) with the addition of our summer, 1999, profile (diamonds - station 153 at 42° 45'N, 136° 03'E).

  19. Summary Nitrite in the water column just above the bottom, in a turbid bottom boundary layer - characteristic of the Ulleung Basin to about 2200 m and of the Primorye and Honshu coasts to about 500 m. Signature of denitrification in the East Sea Proper Water. Reduction of oxygen accompanies the stronger denitrification signature: could the mid-depth oxygen minimum result from sediment processes, especially in the Ulleung Basin? (e.g. suggestion for Pacific by Jahnke and Jackson, 1987) Okhotsk Sea and Bering Sea also sites of denitrification, especially Okhotsk. Major effect on Pacific-wide nitrogen distribution.

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