Anthropogenic CO2 in the Azores region

The AZORES-I cruise was conducted in August 1998, spanning the length of three latitudinal large-scale sections at 22, 28 and 32��W. The oceanic carbon system was oversampled by measuring total alkalinity, total inorganic carbon and pH. It is thus possible to estimate anthropogenic CO2 (CANT) and to investigate its relationship with the main water masses that are present. CANT is calculated using the latest back-calculation techniques: jCT�� and TrOCA methods. Although the two approaches produce similar vertical distributions, the results of the TrOCA method show higher CANT variability and produce higher inventories than those of the jCT�� method. The large proportion of Mediterranean Water found in the northern part of the study area is the main cause of the observed increase northwards of CANT inventories. Changes in CANT inventories between 1981 and 2004 are evaluated using data from the TTO-NAS, OACES-93 and METEOR-60/5 cruises. According to the jCT�� and TrOCA approaches, the average long-term rates of CANT inventory change are 1.32��0.11 mol C m-2 y-1 (P=0.008) and 1.18��0.16 mol C m-2 y-1 (P=0.018), respectively. During the 1993-1998 a significant increase in the CANT storage rate was detected by the jCT�� method. It is thought that this stems directly from the enhanced Labrador Seawater formation after the increased advection observed at the time.

Effects of increased CO2 levels on growth, photosynthesis, ammonium uptake and cell composition in the macroalga Hypnea spinella (Gigartinales, Rhodophyta)

[EN] The red seaweed Hypnea spinella (Gigartinales,��Rhodophyta), was cultured at laboratory scale under three��different CO2 conditions, non-enriched air (360 ppm CO2)and CO2-enriched air at two final concentrations (750 and 1,600 ppm CO2), in order to evaluate the influence of increased CO2 concentrations on growth, photosynthetic��capacity, nitrogen removal efficiency, and chemical cellular��composition. Average specific growth rates of H. spinella treated with 750 and 1,600 ppm CO2-enriched air increased��by 85.6% and 63.2% compared with non-enriched air cultures. CO2 reduction percentages close to 12% were��measured at 750 ppm CO2 with respect to 5% and 7% for��cultures treated with air and 1,600 ppm CO2, respectively.��Maximum photosynthetic rates were enhanced significantly��for high CO2 treatments, showing Pmax values 1.5-fold higher than that for air-treated cultures. N���NH4+ consumption rates were also faster for algae growing at 750 and��1,600 ppm CO2 than that for non-enriched air cultures. As a��consequence of these experimental conditions, soluble��carbohydrates increased and soluble protein contents decreased in algae treated with CO2-enriched air. However,��internal C and N contents remained constant at the different��CO2 concentrations. No significant differences in data��obtained with both elevated CO2 treatments, under the��assayed conditions, indicate that H. spinella is saturated at dissolved inorganic carbon concentrations close by twice��the actual atmospheric levels. The results show that��increased CO2 concentrations might be considered a key��factor in order to improve intensively cultured H. spinella��production yields and carbon and nitrogen bioremediation efficiencies.

Simulations of glacial/interglacial cycles with simple box-models. The ocean CO2 source during deglaciations

M��ster en Oceanograf��a

Emisi��n difusa de CO2 en sistemas volc��nicos activos: implicaciones en la vigilancia volc��nica, la exploraci��n geot��rmica y la emisi��n global de CO2 a la atm��sfera por la actividad volc��nica

Nemesio P��rez Rodr��guez es Coordinador Cient��fico del Instituto Volcanol��gico de Canarias -INVOLCAN-

Air-Sea Interactions of Natural Long-Lived Greenhouse Gases (CO2, N2O, CH4)in a Changing Climate

[EN] Understanding and quantifying ocean-atmosphere exchanges of the long-lived greenhouse gases carbon dioxide (CO2), nitrous oxide (N2O) and methane (CH4) are important for understanding the global biogeochemical cycles of carbon and nitrogen in the context of ongoing global climate change. In this chapter we summarise our current state of knowledge regarding the oceanic distributions, formation and consumption pathways, and oceanic uptake and emissions of CO2, N2O and CH4, with a particular emphasis on the upper ocean. We specifically consider the role of the ocean in regulating the tropospheric content of these important radiative gases in a world in which their tropospheric content is rapidly increasing and estimate the impact of global change on their present and future oceanic uptake and/or emission. Finally, we evaluate the various uncertainties associated with the most commonly used methods for estimating uptake and emission and identify future research needs.

Significance of non���sinking particulate organic carbon and dark CO2 fixation to heterotrophic carbon demand in the mesopelagic northeast Atlantic

<p>[EN] It is generally assumed that sinking particulate organic carbon (POC) constitutes the main source of organic carbon supply to the deep ocean's food webs. However, a major discrepancy between the rates of sinking POC supply (collected with sediment traps) and the prokaryotic organic carbon demand (the total amount of carbon required to sustain the heterotrophic metabolism of the prokaryotes; i.e., production plus respiration, PCD) of deep-water communities has been consistently reported for the dark realm of the global ocean. While the amount of sinking POC flux declines exponentially with depth, the concentration of suspended, buoyant non-sinking POC (nsPOC; obtained with oceanographic bottles) exhibits only small variations with depth in the (sub)tropical Northeast Atlantic. Based on available data for the North Atlantic we show here that the sinking POC flux would contribute only 4&ndash;12% of the PCD in the mesopelagic realm (depending on the primary production rate in surface waters). The amount of nsPOC potentially available to heterotrophic prokaryotes in the mesopelagic realm can be partly replenished by dark dissolved inorganic carbon fixation contributing between 12% to 72% to the PCD daily. Taken together, there is evidence that the mesopelagic microheterotrophic biota is more dependent on the nsPOC pool than on the sinking POC supply. Hence, the enigmatic major mismatch between the organic carbon demand of the deep-water heterotrophic microbiota and the POC supply rates might be substantially smaller by including the potentially available nsPOC and its autochthonous production in oceanic carbon cycling models.</p>

Transporte y almacenamiento de CO2 antropog��nico en el Atl��ntico Norte Tropical

<p>[ES]El aumento de la concentraci&oacute;n de CO2 en la atm&oacute;sfera debido a la emisi&oacute;n por parte de la humanidad esta siendo parcialmente amortiguada gracias a la absorci&oacute;n de ese CO2 por el oc&eacute;ano. El CO2 es captado a trav&eacute;s de la interfase atm&oacute;sfera-oc&eacute;ano y posteriormente la circulaci&oacute;n oce&aacute;nica lo distribuye en el oc&eacute;ano interior. Las mayores tasas de acumulaci&oacute;n de carbono antropog&eacute;nico se detectan en el Atl&aacute;ntico Norte por ello este trabajo est&aacute; enfocado en estudiar c&oacute;mo la circulaci&oacute;n del Atl&aacute;ntico Norte redistribuye este carbono de origen humano en el oc&eacute;ano interior</p>

Planktonic potential CO2 emission calculation: preliminary results by applying an adapted enzymatic methodology to marine ecosystems

<p>[EN]Isocitrate Dehydrogenase (IDH) is a key enzyme in the Krebs cycle, being responsible for the production of one of the three CO2 molecules related to cellular respiration. In order to measure the potential CO2 production linked to the marine planktonic community we have adapted an enzymatic methodology. Preliminary results show that different proportions of autotrophs, heterotrophs and mixotrophs and their metabolic pathways, lead to different relationships between potential CO2 emission and potential O2 consumption during cellular respiration. Although more experiments need to be made, this methodology is leading to a better understanding of cellular respiration in marine samples and their impact on the food chain, vertical Carbon flux and the current sequestering capacity for anthropogenic CO2.</p>