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  • 2020-2024  (9)
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  • 1
    Publication Date: 2023-01-13
    Keywords: DATE/TIME; Gross primary production/Respiration rate ratio; Gross primary production of oxygen; Identification; Net calcification rate of calcium carbonate; Net community calcification rate of calcium carbonate, dark; Net community calcification rate of calcium carbonate, light; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Respiration rate, oxygen; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 216 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-01-13
    Description: The interaction between current flow and topography (e.g., surface ripples) in shallow, permeable coral reef carbonate sediments establishes pressure gradients that increase the rate of sediment-water solute exchange relative to fluid shear along a flat bottom. It is currently unknown how this effect from surface ripples will modify the rate at which the sediment porewater is exposed to future chemical changes in the overlying water column, such as elevated pCO2 that is causing ocean acidification (OA). To address this question, this study used a series of 22-hour incubations in flume aquaria with permeable calcium carbonate sediment communities and examined the interactive effect of pCO2 (400 and 1000 µatm) and surface topography (flat and rippled sediments) on carbonate sediment metabolism and dissolution. According to dissolved oxygen optode image analysis, the presence of surface ripples increased the oxygenated area below the sediment surface by 295% relative to flat sediments. This was reflected in the sediment-to-water column fluxes of dissolved oxygen, where rippled sediments exhibited rates of respiration (R) and gross primary production (GPP) that were ~ 45% and ~ 50% higher, respectively, than flat sediments. An increase in pCO2 shifted the sediments in the flat flumes from net calcifying (Gnet 〉 0) to net dissolving (Gnet 〈 0), an effect that was amplified an additional ~ 60% in rippled sediments. These results suggest that current estimates of coral reef carbonate sediment Gnet may be underestimating the dissolution response to OA where the carbonate sediment environment exhibits ripples in the topography.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-01-02
    Description: Dissolved organic/inorganic carbon and oxygen fluxes from whole sediment core incubations subject to temperature and ocean acidification manipulations. Estuaries make a disproportionately large contribution of dissolved organic carbon (DOC) to the global carbon cycle, but it is unknown how this will change under a future climate. As such, the response of DOC fluxes from microbially dominated unvegetated sediments to individual and combined future climate stressors of warming (from Δ-3 °C to Δ+5 °C on ambient mean temperatures) and ocean acidification (OA, ~2 times the current partial pressure of CO2, pCO2) was investigated ex situ. Warming alone increased sediment heterotrophy, resulting in a proportional increase in sediment DOC uptake, with sediments becoming net sinks of DOC (3.5 to 8.8 mmol-C m-2 d-1) at warmer temperatures (Δ+3 °C and Δ+5 °C, respectively). This temperature response changed under OA conditions, with sediments becoming more autotrophic and a greater sink of DOC (1 to 4 times greater than under current-pCO2). This response was attributed to the stimulation of heterotrophic bacteria with the autochthonous production of labile organic matter by microphytobenthos. Extrapolating these results to the global area of unvegetated subtidal estuarine sediments, the future climate of warming (Δ+3 °C) and OA may decrease the estuarine export of DOC by ~80 % (~150 Tg-C yr-1) and have a disproportionately large impact on the global DOC budget.
    Keywords: AIRICA analyzer (Miranda); Australia; Carbon, inorganic, dissolved; Carbon, organic, dissolved; Clarence_Estuary; DEPTH, sediment/rock; DEPTH, water; estuaries; EXP; Experiment; LDO-probe; Ocean acidification; Oxygen saturation; pH; pH probe; Replicates; Salinity; SALINO; Salinometer; sediment; Surface area; Temperature, water; Temperature sensor; Time in minutes; Time point, descriptive; TOC analyser, Aurora 1030W; Treatment; Volume; warming
    Type: Dataset
    Format: text/tab-separated-values, 1053 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-02-16
    Description: Nitrogen fixation rates (nmol/l/day) were calculated using the 15N-15N enrichments of 3.8 % (Klawonn et al 2015)
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Event label; IN2016_03_CTD102A-N2; IN2016_03_CTD102B-N2; IN2016_03_CTD103A-N2; IN2016_03_CTD103B-N2; IN2016_03_CTD105A-N2; IN2016_03_CTD105B-N2; IN2016_03_CTD106A-N2; IN2016_03_CTD106B-N2; IN2016_03_CTD107A-N2; IN2016_03_CTD107B-N2; IN2016_03_CTD109A-N2; IN2016_03_CTD109B-N2; IN2016_03_CTD110-N2; IN2016_03_CTD114A-N2; IN2016_03_CTD114B-N2; IN2016_03_CTD114C-N2; IN2016_03_CTD115A-N2; IN2016_03_CTD115B-N2; IN2016_03_CTD118B-N2; IN2016_03_CTD118-N2; IN2016_03_CTD119A-N2; IN2016_03_CTD119B-N2; IN2016_03_CTD121A-N2; IN2016_03_CTD121B-N2; IN2016_03_CTD122-N2; IN2016_03_CTD124A-N2; IN2016_03_CTD124B-N2; IN2016_03_CTD125A-N2; IN2016_03_CTD125B-N2; IN2016_03_CTD126-N2; IN2016_03_CTD128A-N2; IN2016_03_CTD128B-N2; IN2016_03_CTD129A-N2; IN2016_03_CTD129B-N2; IN2016_03_CTD12-N2; IN2016_03_CTD131-N2; IN2016_03_CTD132A-N2; IN2016_03_CTD132B-N2; IN2016_03_CTD134A-N2; IN2016_03_CTD134B-N2; IN2016_03_CTD136-N2; IN2016_03_CTD139A-N2; IN2016_03_CTD139B-N2; IN2016_03_CTD13-N2; IN2016_03_CTD140A-N2; IN2016_03_CTD140B-N2; IN2016_03_CTD14-N2; IN2016_03_CTD17B-N2; IN2016_03_CTD17-N2; IN2016_03_CTD18-N2; IN2016_03_CTD20-N2; IN2016_03_CTD21-N2; IN2016_03_CTD23A-N2; IN2016_03_CTD23-N2; IN2016_03_CTD24-N2; IN2016_03_CTD26-N2; IN2016_03_CTD27-N2; IN2016_03_CTD29-N2; IN2016_03_CTD2-N2; IN2016_03_CTD30-N2; IN2016_03_CTD31-N2; IN2016_03_CTD33-N2; IN2016_03_CTD34-N2; IN2016_03_CTD36-N2; IN2016_03_CTD37-N2; IN2016_03_CTD38-N2; IN2016_03_CTD39-N2; IN2016_03_CTD3-N2; IN2016_03_CTD40-N2; IN2016_03_CTD41-N2; IN2016_03_CTD43-N2; IN2016_03_CTD44-N2; IN2016_03_CTD47-N2; IN2016_03_CTD48-N2; IN2016_03_CTD50-N2; IN2016_03_CTD52-N2; IN2016_03_CTD53-N2; IN2016_03_CTD56-N2; IN2016_03_CTD57-N2; IN2016_03_CTD59-N2; IN2016_03_CTD5-N2; IN2016_03_CTD60-N2; IN2016_03_CTD62-N2; IN2016_03_CTD63-N2; IN2016_03_CTD64-N2; IN2016_03_CTD66-N2; IN2016_03_CTD67-N2; IN2016_03_CTD69-N2; IN2016_03_CTD6-N2; IN2016_03_CTD70-N2; IN2016_03_CTD71-N2; IN2016_03_CTD73-N2; IN2016_03_CTD74-N2; IN2016_03_CTD76-N2; IN2016_03_CTD77-N2; IN2016_03_CTD78-N2; IN2016_03_CTD80-N2; IN2016_03_CTD81-N2; IN2016_03_CTD83-N2; IN2016_03_CTD86A-N2; IN2016_03_CTD86B-N2; IN2016_03_CTD86C-N2; IN2016_03_CTD86D-N2; IN2016_03_CTD88-N2; IN2016_03_CTD89-N2; IN2016_03_CTD8-N2; IN2016_03_CTD90A-N2; IN2016_03_CTD90B-N2; IN2016_03_CTD91B-N2; IN2016_03_CTD91-N2; IN2016_03_CTD92-N2; IN2016_03_CTD93B-N2; IN2016_03_CTD93-N2; IN2016_03_CTD95B-N2; IN2016_03_CTD95-N2; IN2016_03_CTD96A-N2; IN2016_03_CTD96B-N2; IN2016_03_CTD96C-N2; IN2016_03_CTD98-N2; IN2016_03_CTD99B-N2; IN2016_03_CTD99-N2; IN2016_03_CTD9-N2; IN2016_04_CTD54-N2; LATITUDE; LONGITUDE; Nitrogen; Nitrogen, total; Nitrogen-15, atmospheric; Nitrogen fixation rate; Sample ID; South Pacific Ocean; Water sample; WS; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 1205 data points
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  • 5
    Publication Date: 2024-03-15
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Oxygen; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Salinity; Temperature, water; Time point, descriptive; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 1824 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-03-15
    Description: Relative to their surface area, estuaries make a disproportionately large contribution of dissolved organic carbon (DOC) to the global carbon cycle, but it is unknown how this will change under a future climate. As such, the response of DOC fluxes from microbially dominated unvegetated sediments to individual and combined future climate stressors of temperature change (from delta −3 to delta +5 °C compared to ambient mean temperatures) and ocean acidification (OA, 2*current CO2 partial pressure, pCO2) was investigated ex situ. Warming alone increased sediment heterotrophy, resulting in a proportional increase in sediment DOC uptake; sediments became net sinks of DOC (3.5 to 8.8 mmol C/m**2/d) at warmer temperatures (delta +3 and delta +5 °C, respectively). This temperature response changed under OA conditions, with sediments becoming more autotrophic and a greater sink of DOC (up to 4* greater than under current pCO2 conditions). This response was attributed to the stimulation of heterotrophic bacteria with the autochthonous production of labile organic matter by microphytobenthos. Extrapolating these results to the global area of unvegetated subtidal estuarine sediments, we find that the future climate of warming (delta +3 °C) and OA may decrease estuarine export of DOC by ∼ 80 % (150 Tg C/yr) and have a disproportionately large impact on the global DOC budget.
    Keywords: AIRICA analyzer (Miranda); Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, flux; Carbon, inorganic, dissolved, flux, standard deviation; Carbon, inorganic, dissolved, standard deviation; Carbon, organic, dissolved; Carbon, organic, dissolved, flux; Carbon, organic, dissolved, flux, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Clarence_River_estuary; Coast and continental shelf; DEPTH, sediment/rock; DEPTH, water; Entire community; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross primary production of oxygen; Gross primary production of oxygen, standard deviation; Laboratory experiment; Net primary production of oxygen; Net primary production of oxygen, standard deviation; Nitrogen, inorganic, dissolved; Nitrogen, inorganic, dissolved, standard deviation; OA-ICC; Ocean Acidification International Coordination Centre; Other studied parameter or process; Oxygen saturation; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Potentiometric; Primary production/Photosynthesis; Production/respiration ratio; Production/respiration ratio, standard deviation; Replicates; Respiration; Respiration rate, oxygen; Respiration rate, oxygen, standard deviation; Salinity; Soft-bottom community; South Pacific; Surface area; Temperate; Temperature; Temperature, water; Temperature, water, standard deviation; Time in minutes; Time point, descriptive; Treatment; Type; Volume
    Type: Dataset
    Format: text/tab-separated-values, 2737 data points
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  • 7
    Publication Date: 2024-05-08
    Description: This global database (CoastDOM v.1) contains both previously published and unpublished measurements of Dissolved organic carbon (DOC), nitrogen (DON) and phosphorus (DOP) in coastal waters. The dataset also contains hydrographic data such as temperature and salinity and, to the extent possible, other biogeochemical variables (e.g., Chlorophyll-a, inorganic nutrients) and the inorganic carbon system (e.g., dissolved inorganic carbon and total alkalinity). The data included were collected from 1978 to 2022 and consist of 62339 data points for DOC, 20360 for DON and 13440 for DOP.
    Keywords: Alkalinity, total; Ammonium; Analytical method; Carbon, inorganic, dissolved; Carbon, organic, dissolved; Carbon, organic, particulate; Chlorophyll a; Coastal waters; Comment; DATE/TIME; DEPTH, water; Dissolved Organic Carbon; Dissolved Organic Matter; dissolved organic nitrogen; dissolved organic phosphorus; ELEVATION; global database;; Hydrogen phosphate; Institution; LATITUDE; Location; LONGITUDE; Nitrate and Nitrite; Nitrogen, organic, dissolved; Nitrogen, particulate; Nitrogen, total dissolved; Phosphorus, organic, dissolved; Phosphorus, particulate; Phosphorus, total dissolved; Principal investigator; Quality flag, alkalinity, total; Quality flag, ammonium; Quality flag, carbon, inorganic, dissolved; Quality flag, carbon, organic, dissolved; Quality flag, carbon, organic, particulate; Quality flag, chlorophyll a; Quality flag, hydrogen phosphate; Quality flag, nitrate and nitrite; Quality flag, nitrogen, particulate; Quality flag, nitrogen, total dissolved; Quality flag, phosphorus, particulate; Quality flag, phosphorus, total dissolved; Reference/source; Salinity; Sample ID; Suspended solids, total; Temperature, water; World Oceans Circulation Experiment (WOCE) quality flags according to Jiang et al. (2022)
    Type: Dataset
    Format: text/tab-separated-values, 1286555 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-02-08
    Description: Nitrous oxide (N2O), like carbon dioxide, is a long-lived greenhouse gas that accumulates in the atmosphere. Over the past 150 years, increasing atmospheric N2O concentrations have contributed to stratospheric ozone depletion1 and climate change2, with the current rate of increase estimated at 2 per cent per decade. Existing national inventories do not provide a full picture of N2O emissions, owing to their omission of natural sources and limitations in methodology for attributing anthropogenic sources. Here we present a global N2O inventory that incorporates both natural and anthropogenic sources and accounts for the interaction between nitrogen additions and the biochemical processes that control N2O emissions. We use bottom-up (inventory, statistical extrapolation of flux measurements, process-based land and ocean modelling) and top-down (atmospheric inversion) approaches to provide a comprehensive quantification of global N2O sources and sinks resulting from 21 natural and human sectors between 1980 and 2016. Global N2O emissions were 17.0 (minimum–maximum estimates: 12.2–23.5) teragrams of nitrogen per year (bottom-up) and 16.9 (15.9–17.7) teragrams of nitrogen per year (top-down) between 2007 and 2016. Global human-induced emissions, which are dominated by nitrogen additions to croplands, increased by 30% over the past four decades to 7.3 (4.2–11.4) teragrams of nitrogen per year. This increase was mainly responsible for the growth in the atmospheric burden. Our findings point to growing N2O emissions in emerging economies—particularly Brazil, China and India. Analysis of process-based model estimates reveals an emerging N2O–climate feedback resulting from interactions between nitrogen additions and climate change. The recent growth in N2O emissions exceeds some of the highest projected emission scenarios3,4, underscoring the urgency to mitigate N2O emissions.
    Type: Article , PeerReviewed
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  • 9
    Publication Date: 2024-02-07
    Description: Coastal ecosystems release or absorb carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), but the net effects of these ecosystems on the radiative balance remain unknown. We compiled a dataset of observations from 738 sites from studies published between 1975 and 2020 to quantify CO2, CH4 and N2O fluxes in estuaries and coastal vegetation in ten global regions. We show that the CO2-equivalent (CO(2)e) uptake by coastal vegetation is decreased by 23-27% due to estuarine CO(2)e outgassing, resulting in a global median net sink of 391 or 444 TgCO(2)e yr(-1) using the 20- or 100-year global warming potentials, respectively. Globally, total coastal CH4 and N2O emissions decrease the coastal CO2 sink by 9-20%. Southeast Asia, North America and Africa are critical regional hotspots of GHG sinks. Understanding these hotspots can guide our efforts to strengthen coastal CO2 uptake while effectively reducing CH4 and N2O emissions. The authors show that estuarine and coastal vegetation are collectively a greenhouse gas (GHG) sink for the atmosphere, but methane and nitrous oxide emissions counteract the carbon dioxide uptake. Critical coastal GHG sink hotspots are identified in Southeast Asia, North America and Africa.
    Type: Article , PeerReviewed
    Format: text
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