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  • Denitrification  (2)
  • 106KL; 138-846; 201-1228; 54-2-PG9; Alkenone, unsaturation index UK'37; AMPH-019G; AMPH01AR; AMPH-025G; AMPHITRITE; Argo; B0406; BC; Box corer; Calculated from UK'37 (Prahl et al., 1988); CARR12; Cocos Ridge; COMPCORE; Composite Core; Core; CORE; DEPTH, sediment/rock; DWBG-140G; DWBG-143; DWBG-144; Eastern Equatorial Pacific; Equatorial East Pacific; Event label; GC; GC_10; Genesis III, RR9702A; Giant piston corer; GPC; Gravity corer; GS7202-18; GS7202-19; GS7202-20; GS7202-22; GS7202-23; GS7202-24; GS7202-38; GS7202-40; GS7202-46; GS7202-52; Hakuho-Maru; HY06; IMAGES VIII - MONA; interpolated; Joides Resolution; KH-03-1; KL; Knorr; KNR176-2; KNR176-2-MC11; KNR176-2-MC14; KNR176-2-MC21; KNR176-2-MC24; KNR176-2-MC28; KNR176-2-MC33; KNR176-2-MC37; KNR176-2-MC4; KNR176-2-MC40; KNR176-2-MC5; KNR176-2-MC7; KNR182-9; KNR182-9-MC10; KNR182-9-MC12; KNR182-9-MC13; KNR182-9-MC14; KNR182-9-MC15; KNR182-9-MC16; KNR182-9-MC17; KNR182-9-MC2; KNR182-9-MC3; KNR182-9-MC4; KNR182-9-MC6; KNR182-9-MC7; KNR182-9-MC8; KNR182-9-MC9; KNR195-5; KNR195-5-MC11; KNR195-5-MC12; KNR195-5-MC16; KNR195-5-MC18; KNR195-5-MC22; KNR195-5-MC25; KNR195-5-MC33; KNR195-5-MC34; KNR195-5-MC38; KNR195-5-MC42; KNR195-5-MC9; Leg138; Leg201; Longitude of event; Marion Dufresne (1995); MD022529; MD02-2529; MD126; ME0005A; ME0005A-04MC4; ME0005A-07MC3; ME0005A-08MC3; ME0005A-14MC2; ME0005A-15MC6; ME0005A-20MC8; ME0005A-21MC3; ME0005A-25MC5; ME0005A-29MC2; ME0005A-35MC1; ME0005A-38MC2; ME0005A-41MC2; Melville; Moana Wave; MUC; MultiCorer; MW8708; MWSC2; MWSC7; NEMO; P6702-11G; P6702-13G; P6702-34G; P6702-4G; P6702-52G; P6702-59; Pacific Ocean; Panama Basin; PC; Peru_Upwelling; Peru1MC3; Peru2MC4; Peru3MC1; Peru4MC2; PERU-AUFTRIEB; Piston corer; Piston corer (BGR type); PLDS-066BX; PLDS-068BX; PLDS-070BX; PLDS-072BX; PLDS-074BX; PLDS-077BX; PLDS-090BX; PLDS-3; Pleiades; PUBS I; RC11; RC1112; RC11-238; RC13; RC13-106; RC13-108; RC13-142; RC18; RC18-46; RC18-48; RC23; RC23-20; Reference/source; Robert Conrad; Roger A. Revelle; RR9702A; RR9702A-62MC3; RR9702A-64MC1; RR9702A-66MC1; RR9702A-68MC3; RR9702A-70MC3; RR9702A-72MC3; RR9702A-74MC2; RR9702A-77MC2; RR9702A-80MC7; RR9702A-82MC; RR9702A-83MC; SC3; SCAN; SCAN-095G; Sea surface temperature, annual mean; SO147; SO147_106KL; Sonne; South-East Pacific; South Pacific Ocean; Temperature, difference; TG7; Thomas Washington; TR163-19; TR163-22; TR163-31; V19; V19-27; V19-28; V19-30; V21; V21-30; Vema; VNTR01; VNTR01-10GC; VNTR01-12GC; VNTR01-19PC; VNTR01-21GC; VNTR01-8PC; VNTR01-9PC; W7706; W7706-40; Wecoma; World Ocean; Y69-71P; YALOC69; Yaquina  (1)
  • 2001-043-3; 2004-024-33; 2006-040-0003; 2006-040-0004; 2008-027-0011; 2008-027-15; 2009-061-0113; 2009-061-111; 2009-061-129; AMOC; BC; Biscaya; Box corer; calculated, 2 sigma; carbonate dissolution; DEPTH, sediment/rock; dolostone; Elevation of event; Event label; GC; Giant box corer; GIK17049-6; GIK17050-1; GIK17051-2; GIK17052-4; GIK17055-1; GIK23517-3; GIK23522-2; GIK23523-3; GIK23528-3; GKG; Gravity corer; Gravity corer (Kiel type); Greenland Sea; Heinrich Stadials; HU2001-043-3; HU2004-024-33; HU2006-040-0003; HU2006-040-0004; HU2006040-006; HU2006040-057; HU2008-027-0011; HU2008-027-15; HU2009-061-0113; HU2009-061-111; HU2009-061-129; Identification; KOL; Labrador Sea; Late Quaternary; Latitude of event; Longitude of event; M11/1; Meteor (1986); Neodymium isotopes; Optional event label; PC; Piston corer; Piston corer (Kiel type); POS210/2; Poseidon; SL; TC; Trigger corer; ε-Neodymium; ε-Neodymium, standard deviation  (1)
Document type
Keywords
Years
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 19 (2005): GB4005, doi:10.1029/2005GB002508.
    Description: On the basis of the normalization to phosphate, a significant amount of nitrate is missing from the deep Bering Sea (BS). Benthic denitrification has been suggested previously to be the dominant cause for the BS nitrate deficit. We measured water column nitrate 15N/14N and 18O/16O as integrative tracers of microbial denitrification, together with pore water-derived benthic nitrate fluxes in the deep BS basin, in order to gain new constraints on the mechanism of fixed nitrogen loss in the BS. The lack of any nitrate isotope enrichment into the deep part of the BS supports the benthic denitrification hypothesis. On the basis of the nitrate deficit in the water column with respect to the adjacent North Pacific and a radiocarbon-derived ventilation age of ∼50 years, we calculate an average deep BS (〉2000 m water depth) sedimentary denitrification rate of ∼230 μmol N m−2 d−1 (or 1.27 Tg N yr−1), more than 3 times higher than high-end estimates of the average global sedimentary denitrification rate for the same depth interval. Pore water-derived estimates of benthic denitrification were variable, and uncertainties in estimates were large. A very high denitrification rate measured from the base of the steep northern slope of the basin suggests that the elevated average sedimentary denitrification rate of the deep Bering calculated from the nitrate deficit is driven by organic matter supply to the base of the continental slope, owing to a combination of high primary productivity in the surface waters along the shelf break and efficient down-slope sediment focusing along the steep continental slopes that characterize the BS.
    Description: This study was supported by NSF grants OCE-0136449 and OCE-9981479 to D. M. S., OCE-0118126 and OCE-0324987 to D. C. M., and DFG grant LE 1326/1-1 to M. F. L. The BS cruise was funded by grant OPP-9912122.
    Keywords: Bering Sea ; Denitrification ; Nitrate isotopes
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: text/plain
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 19 (2004): PA4007, doi:10.1029/2003PA001000.
    Description: An analysis of sedimentary nitrogen isotope records compiled from widely distributed marine environments emphasizes the global synchrony of denitrification changes and provides evidence for a strong temporal coupling of these variations to changes in nitrogen fixation as previously inferred. We explain the global coherence of these records by a simple physical control on the flux of dissolved oxygen to suboxic zones and the coupling to fixation via the supply of phosphorus to diazotrophs in suitable environments. According to our hypothesis, lower glacial-stage sea surface temperature increased oxygen solubility, while stronger winds in high-latitude regions enhanced the rate of thermocline ventilation. The resultant colder, rapidly flushed thermocline lessened the spatial extent of denitrification and, consequently, N fixation. During warm periods, sluggish circulation of warmer, less oxygen rich thermocline waters caused expansion of denitrification zones and a concomitant increase in N fixation. Local fluctuations in export productivity would have modulated this global signal.
    Description: Financial support for this work was provided by the Natural Sciences and Engineering Research Council of Canada and by a WHOI postdoctoral fellowship to MK.
    Keywords: Isotopes ; Fixation ; Denitrification
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-02-02
    Description: This dataset includes the results of the analysis of a set of surface sediment samples recovered from the Labrador Sea. Analysis includes measurement of the radiogenic Nd isotope signatures in the authigenic Fe-Mn oxyhydroxide fraction of the bulk sediment (leachates) and of the totally dissolved residual silicate (detrital) as well as analysis of uncleaned foraminifera.
    Keywords: 2001-043-3; 2004-024-33; 2006-040-0003; 2006-040-0004; 2008-027-0011; 2008-027-15; 2009-061-0113; 2009-061-111; 2009-061-129; AMOC; BC; Biscaya; Box corer; calculated, 2 sigma; carbonate dissolution; DEPTH, sediment/rock; dolostone; Elevation of event; Event label; GC; Giant box corer; GIK17049-6; GIK17050-1; GIK17051-2; GIK17052-4; GIK17055-1; GIK23517-3; GIK23522-2; GIK23523-3; GIK23528-3; GKG; Gravity corer; Gravity corer (Kiel type); Greenland Sea; Heinrich Stadials; HU2001-043-3; HU2004-024-33; HU2006-040-0003; HU2006-040-0004; HU2006040-006; HU2006040-057; HU2008-027-0011; HU2008-027-15; HU2009-061-0113; HU2009-061-111; HU2009-061-129; Identification; KOL; Labrador Sea; Late Quaternary; Latitude of event; Longitude of event; M11/1; Meteor (1986); Neodymium isotopes; Optional event label; PC; Piston corer; Piston corer (Kiel type); POS210/2; Poseidon; SL; TC; Trigger corer; ε-Neodymium; ε-Neodymium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 92 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Kienast, Markus; MacIntyre, G; Dubois, Nathalie; Higginson, S; Normandeau, Claire; Chazen, S; Herbert, Timothy D (2012): Alkenone unsaturation in surface sediments from the eastern equatorial Pacific: Implications for SST reconstructions. Paleoceanography, 27(1), PA1210, https://doi.org/10.1029/2011PA002254
    Publication Date: 2024-02-05
    Description: Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening of the regression at the highest maSSTs is found to be statistically insignificant. For the near-coastal Peru upwelling zone between 11-15°S and 76-79°W, however, we corroborate earlier observations that Uk'37 SST estimates significantly over-estimate maSSTs at many sites. We posit that this is caused either by uncertainties in the determination of maSSTs in this highly dynamic environment, or by biasing of the alkenone paleothermometer toward El Niño events as postulated by Rein et al. (2005).
    Keywords: 106KL; 138-846; 201-1228; 54-2-PG9; Alkenone, unsaturation index UK'37; AMPH-019G; AMPH01AR; AMPH-025G; AMPHITRITE; Argo; B0406; BC; Box corer; Calculated from UK'37 (Prahl et al., 1988); CARR12; Cocos Ridge; COMPCORE; Composite Core; Core; CORE; DEPTH, sediment/rock; DWBG-140G; DWBG-143; DWBG-144; Eastern Equatorial Pacific; Equatorial East Pacific; Event label; GC; GC_10; Genesis III, RR9702A; Giant piston corer; GPC; Gravity corer; GS7202-18; GS7202-19; GS7202-20; GS7202-22; GS7202-23; GS7202-24; GS7202-38; GS7202-40; GS7202-46; GS7202-52; Hakuho-Maru; HY06; IMAGES VIII - MONA; interpolated; Joides Resolution; KH-03-1; KL; Knorr; KNR176-2; KNR176-2-MC11; KNR176-2-MC14; KNR176-2-MC21; KNR176-2-MC24; KNR176-2-MC28; KNR176-2-MC33; KNR176-2-MC37; KNR176-2-MC4; KNR176-2-MC40; KNR176-2-MC5; KNR176-2-MC7; KNR182-9; KNR182-9-MC10; KNR182-9-MC12; KNR182-9-MC13; KNR182-9-MC14; KNR182-9-MC15; KNR182-9-MC16; KNR182-9-MC17; KNR182-9-MC2; KNR182-9-MC3; KNR182-9-MC4; KNR182-9-MC6; KNR182-9-MC7; KNR182-9-MC8; KNR182-9-MC9; KNR195-5; KNR195-5-MC11; KNR195-5-MC12; KNR195-5-MC16; KNR195-5-MC18; KNR195-5-MC22; KNR195-5-MC25; KNR195-5-MC33; KNR195-5-MC34; KNR195-5-MC38; KNR195-5-MC42; KNR195-5-MC9; Leg138; Leg201; Longitude of event; Marion Dufresne (1995); MD022529; MD02-2529; MD126; ME0005A; ME0005A-04MC4; ME0005A-07MC3; ME0005A-08MC3; ME0005A-14MC2; ME0005A-15MC6; ME0005A-20MC8; ME0005A-21MC3; ME0005A-25MC5; ME0005A-29MC2; ME0005A-35MC1; ME0005A-38MC2; ME0005A-41MC2; Melville; Moana Wave; MUC; MultiCorer; MW8708; MWSC2; MWSC7; NEMO; P6702-11G; P6702-13G; P6702-34G; P6702-4G; P6702-52G; P6702-59; Pacific Ocean; Panama Basin; PC; Peru_Upwelling; Peru1MC3; Peru2MC4; Peru3MC1; Peru4MC2; PERU-AUFTRIEB; Piston corer; Piston corer (BGR type); PLDS-066BX; PLDS-068BX; PLDS-070BX; PLDS-072BX; PLDS-074BX; PLDS-077BX; PLDS-090BX; PLDS-3; Pleiades; PUBS I; RC11; RC1112; RC11-238; RC13; RC13-106; RC13-108; RC13-142; RC18; RC18-46; RC18-48; RC23; RC23-20; Reference/source; Robert Conrad; Roger A. Revelle; RR9702A; RR9702A-62MC3; RR9702A-64MC1; RR9702A-66MC1; RR9702A-68MC3; RR9702A-70MC3; RR9702A-72MC3; RR9702A-74MC2; RR9702A-77MC2; RR9702A-80MC7; RR9702A-82MC; RR9702A-83MC; SC3; SCAN; SCAN-095G; Sea surface temperature, annual mean; SO147; SO147_106KL; Sonne; South-East Pacific; South Pacific Ocean; Temperature, difference; TG7; Thomas Washington; TR163-19; TR163-22; TR163-31; V19; V19-27; V19-28; V19-30; V21; V21-30; Vema; VNTR01; VNTR01-10GC; VNTR01-12GC; VNTR01-19PC; VNTR01-21GC; VNTR01-8PC; VNTR01-9PC; W7706; W7706-40; Wecoma; World Ocean; Y69-71P; YALOC69; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 631 data points
    Location Call Number Limitation Availability
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