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  • Dissolved oxygen  (2)
  • 06MT41_3; 224; 230; 237; 286; 290; 293; 297; 316; 318; 321; 323; 333; 335; 368; Agadir Canyon; Aluminium; Amazon Fan; Angola Basin; Angola Benguela Front; Angola Diapir Field; Atlantic Caribbean Margin; BENEFIT/1; Brazil Basin; Calcium; Calculated; Ceara Rise; Center for Marine Environmental Sciences; Central Brazil Basin; Central South Atlantic; Congo Fan; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eastern Niger fan; Elevation of event; Energy dispersive polarization X-ray fluorescence spectrometer (EDP-XRF); Event label; GeoB1412-2; GeoB1501-2; GeoB1505-4; GeoB1511-7; GeoB1512-1; GeoB1606-7; GeoB1608-9; GeoB1612-9; GeoB1703-3; GeoB1716-1; GeoB1720-3; GeoB1728-2; GeoB1808-7; GeoB2019-2; GeoB2102-1; GeoB2108-1; GeoB2112-1; GeoB2116-2; GeoB2119-2; GeoB2125-2; GeoB2208-1; GeoB2216-2; GeoB2306-1; GeoB2307-1; GeoB2709-6; GeoB2712-2; GeoB2715-1; GeoB2719-2; GeoB2723-2; GeoB2724-7; GeoB2727-1; GeoB2802-2; GeoB2806-6; GeoB2808-3; GeoB2813-1; GeoB2825-3; GeoB2906-3; GeoB2909-1; GeoB2910-2; GeoB3601-1; GeoB3605-1; GeoB3709-1; GeoB3711-1; GeoB3803-1; GeoB3804-2; GeoB3809-1; GeoB3906-9; GeoB3910-3; GeoB3911-1; GeoB3914-3; GeoB3915-1; GeoB3936-2; GeoB3939-1; GeoB4226-1; GeoB4304-1; GeoB4306-1; GeoB4310-1; GeoB4312-3; GeoB4319-11; GeoB4407-2; GeoB4409-2; GeoB4411-1; GeoB4417-5; GeoB4418-2; GeoB4420-1; GeoB4421-2; GeoB4502-6; GeoB4901-5; GeoB4903-2; GeoB4904-7; GeoB4905-2; GeoB4908-3; GeoB4911-2; GeoB4915-2; GeoB4916-3; GeoB5132-2; GeoB5201-8; GeoB5556-3; GeoB5903-2; GeoB6005-1; GeoB6105-5; GeoB6201-3; GeoB6203-1; GeoB6207-2; GeoB6210-1; GeoB6212-2; GeoB6214-4; GeoB6221-1; GeoB6230-1; GeoB6312-1; GeoB6313-2; GeoB6322-1; GeoB6340-1; GeoB6409-3; GeoB6417-2; GeoB6421-1; GeoB6427-1; GeoB6509-1; GeoB6518-2; GeoB6908-1; GeoB7001-5; GeoB7002-1; GeoB7417-1; GeoB7423-2; GeoB7430-2; GeoB8206-1; GeoB8305-1; GeoB8324-1; GeoB8329-1; GeoB8402-1; GeoB8493-2; GeoB8501-1; GeoB8505-1; GeoB8506-1; GeoB8522-3; GeoB8524-3; GeoB8626-2; GeoB8630-8; GeoB9501-4; GeoB9508-4; GeoB9512-4; GeoB9531-2; GeoB9533-3; GeoB9536-4; GeoB9538-5; GeoB9601-2; GeoB9602-2; GeoB9624-2; Giant box corer; GKG; Guayana continental slope; Guinea Basin; IOW2; Iron; Latitude of event; ln-Aluminium/Silicon ratio; ln-Iron/Calcium ratio; ln-Iron/Potassium ratio; ln-Titanium/Aluminium ratio; ln-Titanium/Calcium ratio; Longitude of event; M16/1; M16/2; M20/1; M20/2; M22/1; M23/1; M23/2; M23/3; M29/1; M29/2; M29/3; M34/1; M34/2; M34/3; M34/4; M37/1; M38/1; M38/2; M41/1; M41/3; M41/4; M42/4b; M45/1; M45/5a; M46/1; M46/2; M46/3; M46/4; M47/3; M49/3; M49/4; M56/2; M57/1; M57/2; M58/1; M58/2; M65/1; M65/2; MARUM; Mauritania Canyon; Meteor (1986); Midatlantic Ridge; Mid Atlantic Ridge; MUC; MultiCorer; Multicorer with television; Namibia continental slope; NE off San Thome; Northeast Brasilian Margin; Northern Brasil Basin; Northern Cape Basin; off Angola; off Cameroon; off Gabun; off Kunene; off northern Gabun; off Northwest Africa; off NW Africa; Petr Kottsov; POS272; Poseidon; Potassium; PROBOSWA; Santos Plateau; Sierra Leone Rise; Silicon; Slope off Argentina; SO86; Sonne; Southern Cape Basin; Titanium; TVMUC; Uruguay continental margin; Walvis Bay/Namibia; West Angola Basin; Western Equatorial Atlantic  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2018. This is the author's version of the work. It is posted here under a nonexclusive, irrevocable, paid-up, worldwide license granted to WHOI. It is made available for personal use, not for redistribution. The definitive version was published in Limnology and Oceanography-Methods 16 (2018): 323-338, doi:10.1002/lom3.10247.
    Description: We describe a new, autonomous, incubation-based instrument that is deployed in situ to determine rates of gross community respiration and net community production in marine and aquatic ecosystems. During deployments at a coastal pier and in the open ocean, the PHORCYS (PHOtosynthesis and Respiration Comparison-Yielding System) captured dissolved oxygen fluxes over hourly timescales that were missed by traditional methods. The instrument uses fluorescence-quenching optodes fitted into separate light and dark chambers; these are opened and closed with piston-like actuators, allowing the instrument to make multiple, independent rate estimates in the course of each deployment. Consistent with other studies in which methods purporting to measure the same metabolic processes have yielded divergent results, respiration rate estimates from the PHORCYS were systematically higher than those calculated for the same waters using a traditional two-point Winkler titration technique. However, PHORCYS estimates of gross respiration agreed generally with separate incubations in bottles fitted with optode sensor spots. An Appendix describes a new method for estimating uncertainties in metabolic rates calculated from continuous dissolved oxygen data. Multiple successful, unattended deployments of the PHORCYS represent a small step toward fully autonomous observations of community metabolism. Yet the persistence of unexplained disagreements among aquatic metabolic rate estimates — such as those we observed between rates calculated with the PHORCYS and two existing, widely-accepted bottle-based methods — suggests that a new community intercalibration effort is warranted to address lingering sources of error in these critical measurements.
    Description: This research was supported by the U.S. National Science Foundation (awards OCE-1155438 to B.A.S.V.M., J.R.V., and R.G.K., and OCE- 1059884 to B.A.S.V.M.), the Woods Hole Oceanographic Institution through a Cecil and Ida Green Foundation Innovative Technology Award and an Interdisciplinary Science Award, and a U.S. Environmental Protection Agency (EPA) STAR Graduate Fellowship to J.R.C. under Fellowship Assistance Agreement no. FP-91744301-0.
    Keywords: Respiration ; Community metabolism ; Aquatic microbial ecology ; Autonomous instrumentation ; Optodes ; Dissolved oxygen ; Ocean observing
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2013. This is the author's version of the work. It is posted here by permission of Springer for personal use, not for redistribution. The definitive version was published in Estuaries and Coasts 36 (2013): 74-97, doi:10.1007/s12237-012-9560-5.
    Description: Biogeochemical cycles in estuaries are regulated by a diverse set of physical and biological variables that operate over a variety of time scales. Using in situ optical sensors, we conducted a high-frequency time-series study of several biogeochemical parameters at a mooring in central Long Island Sound from May to August 2010. During this period, we documented well-defined diel cycles in nitrate concentration that were correlated to dissolved oxygen, wind stress, tidal mixing, and irradiance. By filtering the data to separate the nitrate time series into various signal components, we estimated the amount of variation that could be ascribed to each process. Primary production and surface wind stress explained 59% and 19%, respectively, of the variation in nitrate concentrations. Less frequent physical forcings, including large-magnitude wind events and spring tides, served to decouple the relationship between oxygen, nitrate, and sunlight on about one-quarter of study days. Daytime nitrate minima and dissolved oxygen maxima occurred nearly simultaneously on the majority (〉 80%) of days during the study period; both were strongly correlated with the daily peak in irradiance. Nighttime nitrate maxima reflected a pattern in which surface-layer stocks were depleted each afternoon and recharged the following night. Changes in nitrate concentrations were used to generate daily estimates of new primary production (182 ± 37 mg C m-2 d-1) and the f-ratio (0.25), i.e., the ratio of production based on nitrate to total production. These estimates, the first of their kind in Long Island Sound, were compared to values of community respiration, primary productivity, and net ecosystem metabolism, which were derived from in situ measurements of oxygen concentration. Daily averages of the three metabolic parameters were 1660 ± 431, 2080 ± 419, and 429 ± 203 mg C m-2 d-1, respectively. While the system remained weakly autotrophic over the duration of the study period, we observed very large day-to-day differences in the f-ratio and in the various metabolic parameters.
    Description: This work was supported by the Yale Institute for Biospheric Studies, the Sounds Conservancy of the Quebec-Labrador Foundation, and the Yale School of Forestry and Environmental Studies Carpenter-Sperry Fund.
    Description: 2014-01-01
    Keywords: Long Island Sound ; Nitrate ; Nitrogen ; New production ; In situ measurements ; Eutrophication ; Dissolved oxygen ; Net ecosystem metabolism ; Wind forcing ; Wind stress ; f-ratio
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Govin, Aline; Holzwarth, Ulrike; Heslop, David; Ford Keeling, Lara; Zabel, Matthias; Mulitza, Stefan; Collins, James A; Chiessi, Cristiano Mazur (2012): Distribution of major elements in Atlantic surface sediments (36°N–49°S): Imprint of terrigenous input and continental weathering. Geochemistry, Geophysics, Geosystems, 13(1), Q01013, https://doi.org/10.1029/2011gc003785
    Publication Date: 2024-02-02
    Description: Numerous studies use major element concentrations measured on continental margin sediments to reconstruct terrestrial climate variations. The choice and interpretation of climate proxies however differ from site to site. Here we map the concentrations of major elements (Ca, Fe, Al, Si, Ti, K) in Atlantic surface sediments (36°N-49°S) to assess the factors influencing the geochemistry of Atlantic hemipelagic sediments and the potential of elemental ratios to reconstruct different terrestrial climate regimes. High concentrations of terrigenous elements and low Ca concentrations along the African and South American margins reflect the dominance of terrigenous input in these regions. Single element concentrations and elemental ratios including Ca (e.g., Fe/Ca) are too sensitive to dilution effects (enhanced biological productivity, carbonate dissolution) to allow reliable reconstructions of terrestrial climate. Other elemental ratios reflect the composition of terrigenous material and mirror the climatic conditions within the continental catchment areas. The Atlantic distribution of Ti/Al supports its use as a proxy for eolian versus fluvial input in regions of dust deposition that are not affected by the input of mafic rock material. The spatial distributions of Al/Si and Fe/K reflect the relative input of intensively weathered material from humid regions versus slightly weathered particles from drier areas. High biogenic opal input however influences the Al/Si ratio. Fe/K is sensitive to the input of mafic material and the topography of Andean river drainage basins. Both ratios are suitable to reconstruct African and South American climatic zones characterized by different intensities of chemical weathering in well-understood environmental settings.
    Keywords: 06MT41_3; 224; 230; 237; 286; 290; 293; 297; 316; 318; 321; 323; 333; 335; 368; Agadir Canyon; Aluminium; Amazon Fan; Angola Basin; Angola Benguela Front; Angola Diapir Field; Atlantic Caribbean Margin; BENEFIT/1; Brazil Basin; Calcium; Calculated; Ceara Rise; Center for Marine Environmental Sciences; Central Brazil Basin; Central South Atlantic; Congo Fan; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eastern Niger fan; Elevation of event; Energy dispersive polarization X-ray fluorescence spectrometer (EDP-XRF); Event label; GeoB1412-2; GeoB1501-2; GeoB1505-4; GeoB1511-7; GeoB1512-1; GeoB1606-7; GeoB1608-9; GeoB1612-9; GeoB1703-3; GeoB1716-1; GeoB1720-3; GeoB1728-2; GeoB1808-7; GeoB2019-2; GeoB2102-1; GeoB2108-1; GeoB2112-1; GeoB2116-2; GeoB2119-2; GeoB2125-2; GeoB2208-1; GeoB2216-2; GeoB2306-1; GeoB2307-1; GeoB2709-6; GeoB2712-2; GeoB2715-1; GeoB2719-2; GeoB2723-2; GeoB2724-7; GeoB2727-1; GeoB2802-2; GeoB2806-6; GeoB2808-3; GeoB2813-1; GeoB2825-3; GeoB2906-3; GeoB2909-1; GeoB2910-2; GeoB3601-1; GeoB3605-1; GeoB3709-1; GeoB3711-1; GeoB3803-1; GeoB3804-2; GeoB3809-1; GeoB3906-9; GeoB3910-3; GeoB3911-1; GeoB3914-3; GeoB3915-1; GeoB3936-2; GeoB3939-1; GeoB4226-1; GeoB4304-1; GeoB4306-1; GeoB4310-1; GeoB4312-3; GeoB4319-11; GeoB4407-2; GeoB4409-2; GeoB4411-1; GeoB4417-5; GeoB4418-2; GeoB4420-1; GeoB4421-2; GeoB4502-6; GeoB4901-5; GeoB4903-2; GeoB4904-7; GeoB4905-2; GeoB4908-3; GeoB4911-2; GeoB4915-2; GeoB4916-3; GeoB5132-2; GeoB5201-8; GeoB5556-3; GeoB5903-2; GeoB6005-1; GeoB6105-5; GeoB6201-3; GeoB6203-1; GeoB6207-2; GeoB6210-1; GeoB6212-2; GeoB6214-4; GeoB6221-1; GeoB6230-1; GeoB6312-1; GeoB6313-2; GeoB6322-1; GeoB6340-1; GeoB6409-3; GeoB6417-2; GeoB6421-1; GeoB6427-1; GeoB6509-1; GeoB6518-2; GeoB6908-1; GeoB7001-5; GeoB7002-1; GeoB7417-1; GeoB7423-2; GeoB7430-2; GeoB8206-1; GeoB8305-1; GeoB8324-1; GeoB8329-1; GeoB8402-1; GeoB8493-2; GeoB8501-1; GeoB8505-1; GeoB8506-1; GeoB8522-3; GeoB8524-3; GeoB8626-2; GeoB8630-8; GeoB9501-4; GeoB9508-4; GeoB9512-4; GeoB9531-2; GeoB9533-3; GeoB9536-4; GeoB9538-5; GeoB9601-2; GeoB9602-2; GeoB9624-2; Giant box corer; GKG; Guayana continental slope; Guinea Basin; IOW2; Iron; Latitude of event; ln-Aluminium/Silicon ratio; ln-Iron/Calcium ratio; ln-Iron/Potassium ratio; ln-Titanium/Aluminium ratio; ln-Titanium/Calcium ratio; Longitude of event; M16/1; M16/2; M20/1; M20/2; M22/1; M23/1; M23/2; M23/3; M29/1; M29/2; M29/3; M34/1; M34/2; M34/3; M34/4; M37/1; M38/1; M38/2; M41/1; M41/3; M41/4; M42/4b; M45/1; M45/5a; M46/1; M46/2; M46/3; M46/4; M47/3; M49/3; M49/4; M56/2; M57/1; M57/2; M58/1; M58/2; M65/1; M65/2; MARUM; Mauritania Canyon; Meteor (1986); Midatlantic Ridge; Mid Atlantic Ridge; MUC; MultiCorer; Multicorer with television; Namibia continental slope; NE off San Thome; Northeast Brasilian Margin; Northern Brasil Basin; Northern Cape Basin; off Angola; off Cameroon; off Gabun; off Kunene; off northern Gabun; off Northwest Africa; off NW Africa; Petr Kottsov; POS272; Poseidon; Potassium; PROBOSWA; Santos Plateau; Sierra Leone Rise; Silicon; Slope off Argentina; SO86; Sonne; Southern Cape Basin; Titanium; TVMUC; Uruguay continental margin; Walvis Bay/Namibia; West Angola Basin; Western Equatorial Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 1687 data points
    Location Call Number Limitation Availability
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