Structural and functional vulnerability to elevated pCO2 in marine benthic communities

The effect of elevated pCO(2)/low pH on marine invertebrate benthic biodiversity, community structure and selected functional responses which underpin ecosystem services (such as community production and calcification) was tested in a medium-term (30 days) mesocosm experiment in June 2010. Standardised intertidal macrobenthic communities, collected (50.3567A degrees N, 4.1277A degrees W) using artificial substrate units (ASUs), were exposed to one of seven pH treatments (8.05, 7.8. 7.6, 7.4, 7.2, 6.8 and 6.0). Community net calcification/dissolution rates, as well as changes in biomass, community structure and diversity, were measured at the end of the experimental period. Communities showed significant changes in structure and reduced diversity in response to reduced pH: shifting from a community dominated by calcareous organisms to one dominated by non-calcareous organisms around either pH 7.2 (number of individuals and species) or pH 7.8 (biomass). These results were supported by a reduced total weight of CaCO3 structures in all major taxa at lowered pH and a switch from net calcification to net dissolution around pH 7.4 (a"broken vertical bar(calc) = 0.78, a"broken vertical bar(ara) = 0.5). Overall community soft tissue biomass did not change with pH and high mortality was observed only at pH 6.0, although molluscs and arthropods showed significant decreases in soft tissue. This study supports and refines previous findings on how elevated pCO(2) can induce changes in marine biodiversity, underlined by differential vulnerability of different phyla. In addition, it shows significant elevated pCO(2)-/low pH-dependent changes in fundamental community functional responses underpinning changes in ecosystem services.

Parental exposure to elevated pCO2 influences the reproductive success of copepods

Substantial variations are reported for egg production and hatching rates of copepods exposed to elevated carbon dioxide concentrations (pCO2). One possible explanation, as found in other marine taxa, is that prior parental exposure to elevated pCO2 (and/or decreased pH) affects reproductive performance. Previous studies have adopted two distinct approaches, either (1) expose male and female copepoda to the test pCO2/pH scenarios, or (2) solely expose egg-laying females to the tests. Although the former approach is more realistic, the majority of studies have used the latter approach. Here, we investigated the variation in egg production and hatching success of Acartia tonsa between these two experimental designs, across five different pCO2 concentrations (385–6000 µatm pCO2). In addition, to determine the effect of pCO2 on the hatching success with no prior parental exposure, eggs produced and fertilized under ambient conditions were also exposed to these pCO2 scenarios. Significant variations were found between experimental designs, with approach (1) resulting in higher impacts; here >20% difference was seen in hatching success between experiments at 1000 µatm pCO2 scenarios (2100 year scenario), and >85% at 6000 µatm pCO2. This study highlights the potential to misrepresent the reproductive response of a species to elevated pCO2 dependent on parental exposure.

Synchronous records of pCO2 and Δ14C suggest rapid, ocean-derived pCO2 fluctuations at the onset of Younger Dryas

Just before the onset of the Younger Dryas (YD) cold event, several stomatal proxy-based pCO2 records have shown a sharp increase in atmospheric CO2 concentration (pCO2) of between ca 50 and 100 ppm, followed by a rapid decrease of similar or even larger magnitude. Here we compare one of these records, a high-resolution pCO2 record from southern Sweden, with the IntCal13 record of radiocarbon (Δ14C). The two records show broadly synchronous fluctuations at the YD onset. Specifically, the IntCal13 record documents decreasing Δ14C just before the YD onset when pCO2 peaks, consistent with a source of “old” CO2 from the deep ocean. We propose that this fluctuation occurred due to a major ocean flushing event. The cause of the flushing event remains speculative but could be related to the hypothesis of the glacial ocean as a thermobaric capacitor. We confirm that the earth system can produce such large multi-decadal timescale fluctuations in pCO2 through simulating an artificial ocean flushing event with the GENIE Earth System Model. We suggest that sharp transitions of pCO2 may have remained undetected so far in ice cores due to inter-firn gas exchange and time-averaging. The stomatal proxy record is a powerful complement to the ice core records for the study of rapid climate change.

Structural and chemical characterization of corals grown under present day and naturally elevated pCO2 conditions in Papua New Guinea - a window into the future

Dissertação de mestrado, Biologia Marinha, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2015

Underway O2/Ar-estiment net community production across the Kuroshio Extension and impact on winter pCO2 drawdown

Senior thesis written for Oceanography 445

Diferencia venoarterial de PCO2 como predictor de disfunción miocárdica en pacientes pediátricos con sepsis severa y choque séptico

El objetivo de este estudio, es determinar la capacidad de la diferencia venoarterial de de pCO2, como predictor de disfunción miocárdica en pacientes pediátricos con sepsis severa y choque séptico en la Unidad de Cuidado Intensivo Pediátrico de la Fundación Cardio Infantil. El documento eviado corresponde a un informe parcial de un estudio en curso en la Fundación CardioInfantil.

Diferencia venoarterial de Pco2 como predictor de disfunción miocárdica en niños con sepsis severa y choque séptico.

Introducción: La sepsis es una de las principales causas de morbilidad y mortalidad en la población pediátrica a nivel mundial, siendo la disminución del gasto cardiaco uno de los principales factores asociados a mortalidad. Se ha planteado la diferencia venoarterial de pCO2 como predictor de la función miocárdica en pacientes con sepsis, sin embargo hasta el momento no hay estudios en la población pediátrica que lo evalúen. Objetivo: Determinar la capacidad predictora y las características operativas de la diferencia venoarterial de pCO2, como predictor de disfunción miocárdica en pacientes pediátricos con sepsis severa y choque séptico. Métodos: Para alcanzar los objetivos del estudio, se llevo a cabo un estudio prospectivo de pruebas diagnósticas. Se realizó ecocardiograma y diferencia venoarterial de pCO2 en cada paciente, posteriormente se calculó las características operativas de la diferencia venoarterial de pCO2 para determinar su utilidad. Resultados: Se incluyeron 71 pacientes. La mediana de la diferencia venoarterial de pCO2 no fue significativamente mayor en los pacientes que tuvieron disfunción cardiaca en el ecocardiograma en comparación con los que no tuvieron disfunción. Se encontró una relación estadísticamente significativa de valores de 1,5 a 2,1 mmHg, como predictor negativo de disfunción miocárdica con una sensibilidad de 100% y una especificidad de 88%. Conclusiones: La diferencia venoarterial de pCO2 requiere de estudios mas extensos para determinar la probabilidad como predictor de disfunción miocárdica en pacientes pediátricos con sepsis severa y choque séptico, incluso cuando otros biomarcadores se encuentran dentro de límites normales.

Valores sanguíneos de pH, pCO2, pO2, e HCO3 e proteinograma sérico de cabritos de raça Saanem do nascimento aos quatro meses de idade

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Estimating the monthly pCO2 distribution in the North Atlantic using a self-organizing neural network

[EN] Here we present monthly, basin-wide maps of the partial pressure of carbon dioxide (pCO2) for the North Atlantic on a latitude by longitude grid for years 2004 through 2006 inclusive. The maps have been computed using a neural network technique which reconstructs the non-linear relationships between three biogeochemical parameters and marine pCO2. A self organizing map (SOM) neural network has been trained using 389 000 triplets of the SeaWiFSMODIS chlorophyll-a concentration, the NCEP/NCAR reanalysis sea surface temperature, and the FOAM mixed layer depth. The trained SOM was labelled with 137 000 underway pCO2 measurements collected in situ during 2004, 2005 and 2006 in the North Atlantic, spanning the range of 208 to 437atm. The root mean square error (RMSE) of the neural network fit to the data is 11.6?atm, which equals to just above 3 per cent of an average pCO2 value in the in situ dataset. The seasonal pCO2 cycle as well as estimates of the interannual variability in the major biogeochemical provinces are presented and discussed. High resolution combined with basin-wide coverage makes the maps a useful tool for several applications such as the monitoring of basin-wide air-sea CO2 fluxes or improvement of seasonal and interannual marine CO2 cycles in future model predictions. The method itself is a valuable alternative to traditional statistical modelling techniques used in geosciences.