Shallow remineralization in the Sargasso Sea estimated from seasonal variations in oxygen, dissolved inorganic carbon and nitrate

S. Ono, A. Ennyu, R. G. Najjar, N. R. Bates

Research output: Contribution to journalArticle

38 Citations (Scopus)

Abstract

A diagnostic model of the mean annual cycles of oxygen, dissolved inorganic carbon (DIC) and nitrate below the mixed layer at the Bermuda Atlantic Time-Series Study (BATS) site is presented and used to estimate organic matter remineralization in the seasonal thermocline. The model includes lateral and vertical advection as well as vertical diffusion, which are found to be significant components of the seasonal budgets of oxygen, DIC and nitrate. The vertical and seasonal variation of the remineralization rates deduced from the oxygen and DIC distributions are very similar. Both locate the spring-summer community compensation depth at ∼ 85m and the remineralization rate maximum at ∼ 120 m; nitrate-based estimates of these depths are about 40m greater. Remineralization rates based on oxygen, DIC and nitrate all show the seasonal maximum to occur in the late spring, presumably reflecting the decomposition of organic matter formed during the spring bloom. The remineralization rate integrated between 100 and 250 m and between mid-April and mid-December is estimated to be 2.08 ± 0.38 mol O2 m-2, 1.53 ± 0.35 mol Cm-2 and 0.080 ± 0.046 mol Nm-2. These imply remineralization ratios of O2 : C = 1.4 ± 0.40 and C : N = 19 ± 12. The former agrees well with the canonical Redfield ratio and the latter is significantly larger. The analysis is consistent with the export and remineralization of nitrogen-poor organic matter from surface waters.

Original languageEnglish (US)
Pages (from-to)1567-1582
Number of pages16
JournalDeep-Sea Research Part II: Topical Studies in Oceanography
Volume48
Issue number8-9
DOIs
StatePublished - May 24 2001

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remineralization
dissolved inorganic carbon
seasonal variation
nitrate
oxygen
organic matter
Redfield ratio
sea
thermocline
annual cycle
mixed layer
algal bloom
advection
time series
decomposition
surface water
rate
nitrogen
summer

All Science Journal Classification (ASJC) codes

  • Oceanography

Cite this

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title = "Shallow remineralization in the Sargasso Sea estimated from seasonal variations in oxygen, dissolved inorganic carbon and nitrate",
abstract = "A diagnostic model of the mean annual cycles of oxygen, dissolved inorganic carbon (DIC) and nitrate below the mixed layer at the Bermuda Atlantic Time-Series Study (BATS) site is presented and used to estimate organic matter remineralization in the seasonal thermocline. The model includes lateral and vertical advection as well as vertical diffusion, which are found to be significant components of the seasonal budgets of oxygen, DIC and nitrate. The vertical and seasonal variation of the remineralization rates deduced from the oxygen and DIC distributions are very similar. Both locate the spring-summer community compensation depth at ∼ 85m and the remineralization rate maximum at ∼ 120 m; nitrate-based estimates of these depths are about 40m greater. Remineralization rates based on oxygen, DIC and nitrate all show the seasonal maximum to occur in the late spring, presumably reflecting the decomposition of organic matter formed during the spring bloom. The remineralization rate integrated between 100 and 250 m and between mid-April and mid-December is estimated to be 2.08 ± 0.38 mol O2 m-2, 1.53 ± 0.35 mol Cm-2 and 0.080 ± 0.046 mol Nm-2. These imply remineralization ratios of O2 : C = 1.4 ± 0.40 and C : N = 19 ± 12. The former agrees well with the canonical Redfield ratio and the latter is significantly larger. The analysis is consistent with the export and remineralization of nitrogen-poor organic matter from surface waters.",
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Shallow remineralization in the Sargasso Sea estimated from seasonal variations in oxygen, dissolved inorganic carbon and nitrate. / Ono, S.; Ennyu, A.; Najjar, R. G.; Bates, N. R.

In: Deep-Sea Research Part II: Topical Studies in Oceanography, Vol. 48, No. 8-9, 24.05.2001, p. 1567-1582.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Shallow remineralization in the Sargasso Sea estimated from seasonal variations in oxygen, dissolved inorganic carbon and nitrate

AU - Ono, S.

AU - Ennyu, A.

AU - Najjar, R. G.

AU - Bates, N. R.

PY - 2001/5/24

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N2 - A diagnostic model of the mean annual cycles of oxygen, dissolved inorganic carbon (DIC) and nitrate below the mixed layer at the Bermuda Atlantic Time-Series Study (BATS) site is presented and used to estimate organic matter remineralization in the seasonal thermocline. The model includes lateral and vertical advection as well as vertical diffusion, which are found to be significant components of the seasonal budgets of oxygen, DIC and nitrate. The vertical and seasonal variation of the remineralization rates deduced from the oxygen and DIC distributions are very similar. Both locate the spring-summer community compensation depth at ∼ 85m and the remineralization rate maximum at ∼ 120 m; nitrate-based estimates of these depths are about 40m greater. Remineralization rates based on oxygen, DIC and nitrate all show the seasonal maximum to occur in the late spring, presumably reflecting the decomposition of organic matter formed during the spring bloom. The remineralization rate integrated between 100 and 250 m and between mid-April and mid-December is estimated to be 2.08 ± 0.38 mol O2 m-2, 1.53 ± 0.35 mol Cm-2 and 0.080 ± 0.046 mol Nm-2. These imply remineralization ratios of O2 : C = 1.4 ± 0.40 and C : N = 19 ± 12. The former agrees well with the canonical Redfield ratio and the latter is significantly larger. The analysis is consistent with the export and remineralization of nitrogen-poor organic matter from surface waters.

AB - A diagnostic model of the mean annual cycles of oxygen, dissolved inorganic carbon (DIC) and nitrate below the mixed layer at the Bermuda Atlantic Time-Series Study (BATS) site is presented and used to estimate organic matter remineralization in the seasonal thermocline. The model includes lateral and vertical advection as well as vertical diffusion, which are found to be significant components of the seasonal budgets of oxygen, DIC and nitrate. The vertical and seasonal variation of the remineralization rates deduced from the oxygen and DIC distributions are very similar. Both locate the spring-summer community compensation depth at ∼ 85m and the remineralization rate maximum at ∼ 120 m; nitrate-based estimates of these depths are about 40m greater. Remineralization rates based on oxygen, DIC and nitrate all show the seasonal maximum to occur in the late spring, presumably reflecting the decomposition of organic matter formed during the spring bloom. The remineralization rate integrated between 100 and 250 m and between mid-April and mid-December is estimated to be 2.08 ± 0.38 mol O2 m-2, 1.53 ± 0.35 mol Cm-2 and 0.080 ± 0.046 mol Nm-2. These imply remineralization ratios of O2 : C = 1.4 ± 0.40 and C : N = 19 ± 12. The former agrees well with the canonical Redfield ratio and the latter is significantly larger. The analysis is consistent with the export and remineralization of nitrogen-poor organic matter from surface waters.

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