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18 results on '"I. R. Santos"'

1. Hypersaline tidal flats as important 'blue carbon' systems: a case study from three ecosystems

Author

D. R. Brown, H. Marotta, R. B. Peixoto, A. Enrich-Prast, G. C. Barroso, M. L. G. Soares, W. Machado, A. Pérez, J. M. Smoak, L. M. Sanders, S. Conrad, J. Z. Sippo, I. R. Santos, D. T. Maher, and C. J. Sanders

Subjects
Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Abstract

Hypersaline tidal flats (HTFs) are coastal ecosystems with freshwater deficits often occurring in arid or semi-arid regions near mangrove supratidal zones with no major fluvial contributions. Here, we estimate that organic carbon (OC), total nitrogen (TN) and total phosphorus (TP) were buried at rates averaging 21 (±6), 1.7 (±0.3) and 1.4 (±0.3) gm-2yr-1, respectively, during the previous century in three contrasting HTF systems, one in Brazil (eutrophic) and two in Australia (oligotrophic). Although these rates are lower than those from nearby mangrove, saltmarsh and seagrass systems, the importance of HTFs as sinks for OC, TN and TP may be significant given their extensive coverage. Despite the measured short-term variability between net air–saltpan CO2 influx and emission estimates found during the dry and wet season in the Brazilian HTF, the only site with seasonal CO2 flux measurements, the OC sedimentary profiles over several decades suggest efficient OC burial at all sites. Indeed, the stable isotopes of OC and TN (δ13C and δ15N) along with C:N ratios show that microphytobenthos are the major source of the buried OC in these HTFs. Our findings highlight a previously unquantified carbon as well as a nutrient sink and suggest that coastal HTF ecosystems could be included in the emerging blue carbon framework.

Published
2021
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2. Reconstructing extreme climatic and geochemical conditions during the largest natural mangrove dieback on record

Author

J. Z. Sippo, I. R. Santos, C. J. Sanders, P. Gadd, Q. Hua, C. E. Lovelock, N. S. Santini, S. G. Johnston, Y. Harada, G. Reithmeir, and D. T. Maher

Subjects
Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Abstract

A massive mangrove dieback event occurred in 2015–2016 along ∼1000 km of pristine coastline in the Gulf of Carpentaria, Australia. Here, we use sediment and wood chronologies to gain insights into geochemical and climatic changes related to this dieback. The unique combination of low rainfall and low sea level observed during the dieback event had been unprecedented in the preceding 3 decades. A combination of iron (Fe) chronologies in wood and sediment, wood density and estimates of mangrove water use efficiency all imply lower water availability within the dead mangrove forest. Wood and sediment chronologies suggest a rapid, large mobilization of sedimentary Fe, which is consistent with redox transitions promoted by changes in soil moisture content. Elemental analysis of wood cross sections revealed a 30- to 90-fold increase in Fe concentrations in dead mangroves just prior to their mortality. Mangrove wood uptake of Fe during the dieback is consistent with large apparent losses of Fe from sediments, which potentially caused an outwelling of Fe to the ocean. Although Fe toxicity may also have played a role in the dieback, this possibility requires further study. We suggest that differences in wood and sedimentary Fe between living and dead forest areas reflect sediment redox transitions that are, in turn, associated with regional variability in groundwater flows. Overall, our observations provide multiple lines of evidence that the forest dieback was driven by low water availability coinciding with a strong El Niño–Southern Oscillation (ENSO) event and was associated with climate change.

Published
2020
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3. Role of carbonate burial in Blue Carbon budgets

Author

V. Saderne, N. R. Geraldi, P. I. Macreadie, D. T. Maher, J. J. Middelburg, O. Serrano, H. Almahasheer, A. Arias-Ortiz, M. Cusack, B. D. Eyre, J. W. Fourqurean, H. Kennedy, D. Krause-Jensen, T. Kuwae, P. S. Lavery, C. E. Lovelock, N. Marba, P. Masqué, M. A. Mateo, I. Mazarrasa, K. J. McGlathery, M. P. J. Oreska, C. J. Sanders, I. R. Santos, J. M. Smoak, T. Tanaya, K. Watanabe, and C. M. Duarte

Subjects
Science
Abstract

Calcium carbonates (CaCO3) often accumulate in mangrove and seagrass sediments. Here the authors conducted a meta-analysis of inorganic carbon burial rates in mangrove and seagrass sediments and found that CaCO3 burial contributes to Blue Carbon ecosystems’ capacity to offset sea-level rise without undermining the role as CO2 sinks.

Published
2019
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4. Technical note: Coupling infrared gas analysis and cavity ring down spectroscopy for autonomous, high-temporal-resolution measurements of DIC and δ13C–DIC

Author

M. Call, K. G. Schulz, M. C. Carvalho, I. R. Santos, and D. T. Maher

Subjects
Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Abstract

A new approach to autonomously determine concentrations of dissolved inorganic carbon (DIC) and its carbon stable isotope ratio (δ13C–DIC) at high temporal resolution is presented. The simple method requires no customised design. Instead it uses two commercially available instruments currently used in aquatic carbon research. An inorganic carbon analyser utilising non-dispersive infrared detection (NDIR) is coupled to a Cavity Ring-down Spectrometer (CRDS) to determine DIC and δ13C–DIC based on the liberated CO2 from acidified aliquots of water. Using a small sample volume of 2 mL, the precision and accuracy of the new method was comparable to standard isotope ratio mass spectrometry (IRMS) methods. The system achieved a sampling resolution of 16 min, with a DIC precision of ±1.5 to 2 µmol kg−1 and δ13C–DIC precision of ±0.14 ‰ for concentrations spanning 1000 to 3600 µmol kg−1. Accuracy of 0.1 ± 0.06 ‰ for δ13C–DIC based on DIC concentrations ranging from 2000 to 2230 µmol kg−1 was achieved during a laboratory-based algal bloom experiment. The high precision data that can be autonomously obtained by the system should enable complex carbonate system questions to be explored in aquatic sciences using high-temporal-resolution observations.

Published
2017
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5. Seasonal, daily and diel N2 effluxes in permeable carbonate sediments

Author

B. D. Eyre, I. R. Santos, and D. T. Maher

Subjects
Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Abstract

Benthic metabolism and inorganic nitrogen and N2 flux rates (denitrification) were measured in permeable carbonate sands from Heron Island (Great Barrier Reef). Some of the N2 flux rates were among the highest measured in sediments. All benthic fluxes showed a significant difference between seasons with higher rates in summer and late summer. There was no distinct response of the benthic system to mass coral spawning. Instead, changes in benthic fluxes over 12 days in summer appear to be driven by tidal changes in water depth and associated changes in phytosynthetically active radiation reaching the sediments. Dark N2 fluxes were strongly correlated to benthic oxygen consumption across all sites and seasons (r2 = 0.63; p < 0.005; slope = 0.035). However, there were seasonal differences with a steeper slope in summer than winter, reflecting either more efficient coupling between respiration and nitrification–denitrification at higher temperatures or different sources of organic matter. Adding data from published studies on carbonate sands revealed two slopes in the dark N2 flux versus benthic oxygen consumption relationship. The lower slope (0.035) was most likely due to high carbon : nitrogen (C : N) organic matter from coral reefs, and associated assimilation of nitrogen by heterotrophic bacteria including enhanced heterotrophic N-fixation, but competition by benthic microalgae or inefficient coupling between respiration and nitrification–denitrification cannot be excluded. The steeper slope (0.089) was most likely due to respiration being driven by low C : N phytodetritus. If the different slopes were driven by the sources of organic matter, then global estimates of continental shelf denitrification are probably about right. In contrast, global estimates of continental shelf denitrification may be over-estimated if the low slope was due to inefficient coupling between respiration and nitrification–denitrification and also due to reduced N2 effluxes in the light associated with competition by benthic microalgae for nitrogen and N-fixation.

Published
2013
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6. Groundwater and porewater as major sources of alkalinity to a fringing coral reef lagoon (Muri Lagoon, Cook Islands)

Author

T. Cyronak, I. R. Santos, D. V. Erler, and B. D. Eyre

Subjects
Ecology, QH540-549.5, Life, QH501-531, Geology, QE1-996.5
Abstract

To better predict how ocean acidification will affect coral reefs, it is important to understand how biogeochemical cycles on reefs alter carbonate chemistry over various temporal and spatial scales. This study quantifies the contribution of shallow porewater exchange (as quantified from advective chamber incubations) and fresh groundwater discharge (as traced by 222Rn) to total alkalinity (TA) dynamics on a fringing coral reef lagoon along the southern Pacific island of Rarotonga over a tidal and diel cycle. Benthic alkalinity fluxes were affected by the advective circulation of water through permeable sediments, with net daily flux rates of carbonate alkalinity ranging from −1.55 to 7.76 mmol m−2 d−1, depending on the advection rate. Submarine groundwater discharge (SGD) was a source of TA to the lagoon, with the highest flux rates measured at low tide, and an average daily TA flux of 1080 mmol m−2 d−1 at the sampling site. Both sources of TA were important on a reef-wide basis, although SGD acted solely as a delivery mechanism of TA to the lagoon, while porewater advection was either a sink or source of TA dependent on the time of day. This study describes overlooked sources of TA to coral reef ecosystems that can potentially alter water column carbonate chemistry. We suggest that porewater and groundwater fluxes of TA should be taken into account in ocean acidification models in order to properly address changing carbonate chemistry within coral reef ecosystems.

Published
2013
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7. The contribution of groundwater discharge to the overall water budget of two typical Boreal lakes in Alberta/Canada estimated from a radon mass balance

Author

A. Schmidt, J. J. Gibson, I. R. Santos, M. Schubert, K. Tattrie, and H. Weiss

Subjects
Technology, Environmental technology. Sanitary engineering, TD1-1066, Geography. Anthropology. Recreation, Environmental sciences, GE1-350
Abstract

Radon-222, a naturally-occurring radioisotope with a half-life of 3.8 days, was used to estimate groundwater discharge to small lakes in wetland-dominated basins in the vicinity of Fort McMurray, Canada. This region is under significant water development pressure including both oil sands mining and in situ extraction. Field investigations were carried out in March and July 2008 to measure radon-222 distributions in the water column of two lakes as a tracer of groundwater discharge. Radon concentrations in these lakes ranged from 0.5 to 72 Bq/m3, while radon concentrations in groundwaters ranged between 2000 and 8000 Bq/m3. A radon mass balance, used in comparison with stable isotope mass balance, suggested that the two lakes under investigation had quite different proportions of annual groundwater inflow (from 0.5% to about 14% of the total annual water inflow). Lower discharge rates were attributed to a larger drainage area/lake area ratio which promotes greater surface connectivity. Interannual variability in groundwater proportions is expected despite an implied seasonal constancy in groundwater discharge rates. Our results demonstrate that a combination of stable isotope and radon mass balance approaches provides information on flowpath partitioning that is useful for evaluating surface-groundwater connectivity and acid sensitivity of individual water bodies of interest in the Alberta Oil Sands Region.

Published
2010

12. Seasonal, daily and diel N2 effluxes in permeable carbonate sediments

Author

B. D. Eyre, I. R. Santos, and D. T. Maher

Subjects
lcsh:Geology, lcsh:QH501-531, lcsh:QH540-549.5, lcsh:QE1-996.5, fungi, lcsh:Life, lcsh:Ecology, geographic locations
Abstract

Benthic metabolism and inorganic nitrogen and N2 flux rates (denitrification) were measured in permeable carbonate sands from Heron Island (Great Barrier Reef). Some of the N2 flux rates were among the highest measured in sediments. All benthic fluxes showed a significant difference between seasons with higher rates in summer and late summer. There was no distinct response of the benthic system to mass coral spawning. Instead, changes in benthic fluxes over 12 days in summer appear to be driven by tidal changes in water depth and associated changes in phytosynthetically active radiation reaching the sediments. Dark N2 fluxes were strongly correlated to benthic oxygen consumption across all sites and seasons (r2 = 0.63; p < 0.005; slope = 0.035). However, there were seasonal differences with a steeper slope in summer than winter, reflecting either more efficient coupling between respiration and nitrification–denitrification at higher temperatures or different sources of organic matter. Adding data from published studies on carbonate sands revealed two slopes in the dark N2 flux versus benthic oxygen consumption relationship. The lower slope (0.035) was most likely due to high carbon : nitrogen (C : N) organic matter from coral reefs, and associated assimilation of nitrogen by heterotrophic bacteria including enhanced heterotrophic N-fixation, but competition by benthic microalgae or inefficient coupling between respiration and nitrification–denitrification cannot be excluded. The steeper slope (0.089) was most likely due to respiration being driven by low C : N phytodetritus. If the different slopes were driven by the sources of organic matter, then global estimates of continental shelf denitrification are probably about right. In contrast, global estimates of continental shelf denitrification may be over-estimated if the low slope was due to inefficient coupling between respiration and nitrification–denitrification and also due to reduced N2 effluxes in the light associated with competition by benthic microalgae for nitrogen and N-fixation.

Published
2018

13. Poster session 3

Author

O. Nanka, E. Krejci, Z. Pesevski, D. Sedmera, N. Smart, A. Rossdeutsch, K. N. Dube, J. Riegler, A. N. Price, A. Taylor, V. Muthurangu, M. Turner, M. F. Lythgoe, P. R. Riley, S. Kryvorot, T. Vladimirskaya, I. Shved, M. Schwarzl, S. Seiler, S. Huber, P. Steendijk, H. Maechler, M. Truschnig-Wilders, B. Pieske, H. Post, C. Caprio, A. Baldini, E. Chiavacci, L. Dolfi, L. Verduci, F. Meghini, F. Cremisi, L. Pitto, T.-C. Kuan, M.-C. Chen, T.-H. Yang, W.-T. Wu, C. S. Lin, H. Rai, S. Kumar, A. K. Sharma, S. Mastana, A. Kapoor, C. M. Pandey, S. Agrawal, N. Sinha, E. H. Orlowska-Baranowska, G. Placha, J. Gora, R. Baranowski, E. Abramczuk, T. Hryniewiecki, Z. Gaciong, J. J. W. Verschuren, J. A. M. Wessels, S. Trompet, D. J. Stott, N. Sattar, B. Buckley, H. J. Guchelaar, J. W. Jukema, M. Gharanei, A. Hussain, C. J. Mee, H. L. Maddock, W. J. Wijnen, S. Van Den Oever, I. Van Der Made, M. Hiller, A. J. Tijsen, Y. M. Pinto, E. E. Creemers, S. U. Y. Nikulina, A. Chernova, A. Petry, T. Rzymski, D. Kracun, F. Riess, L. Pike, A. L. Harris, A. Gorlach, R. Katare, A. Oikawa, F. Riu, A. P. Beltrami, D. Cesseli, C. Emanueli, P. Madeddu, T. Zaglia, G. Milan, M. Franzoso, P. Pesce, C. Sarais, M. Sandri, M. Mongillo, T. J. Butler, A.-M. L. Seymour, D. Ashford, F. Jaffre, M. Bussen, I. Flohrschutz, G. R. Martin, S. Engelhardt, G. Kararigas, B. T. Nguyen, H. Jarry, V. Regitz-Zagrosek, M. Van Bilsen, A. Daniels, C. Munts, B. J. A. Janssen, G. J. Van Der Vusse, F. A. Van Nieuwenhoven, C. Montalvo, A. V. Villar, D. Merino, R. Garcia, M. Llano, M. Ares, M. A. Hurle, J. F. Nistal, A. Dembinska-Kiec, B. K. W. Beata Kiec-Wilk, A. P. Anna Polus, U. C. Urszula Czech, T. K. Tatiana Konovaleva, G. S. Gerd Schmitz, L. Bertrand, M. Balteau, A. Timmermans, B. Viollet, K. Sakamoto, O. Feron, S. Horman, J. L. Vanoverschelde, C. Beauloye, C. De Meester, E. Martinez, R. Martin, M. Miana, R. Jurado, N. Gomez-Hurtado, M. V. Bartolome, J. A. San Roman, V. Lahera, M. L. Nieto, V. Cachofeiro, F. Rochais, R. Sturny, K. Mesbah, L. Miquerol, R. G. Kelly, S. Messaoudi, B. Gravez, A. Tarjus, V. Pelloux, J. L. Samuel, C. Delcayre, J. M. Launay, K. Clement, N. Farman, F. Jaisser, L. Hadyanto, C. Castellani, G. Vescovo, B. Ravara, R. Tavano, M. Pozzobon, P. De Coppi, E. Papini, R. Vettor, G. Thiene, A. Angelini, M. Meloni, A. Caporali, D. Cesselli, O. Fortunato, E. Avolio, R. Schindler, S. Simrick, T. Brand, N. S. Smart, A. Herman, S. Roura Ferrer, J. Rodriguez Bago, C. Soler-Botija, J. M. Pujal, C. Galvez-Monton, C. Prat-Vidal, A. Llucia-Valldeperas, J. Blanco, A. Bayes-Genis, G. Foldes, M. Maxime, N. N. Ali, M. D. Schneider, S. E. Harding, C. Reni, G. Mangialardi, A. De Pauw, B. Sekkali, A. Friart, H. Ding, A. Graffeuil, D. Catalucci, J. L. Balligand, F. Azibani, F. Tournoux, S. Schlossarek, E. Polidano, L. Fazal, R. Merval, L. Carrier, C. Chatziantoniou, B. Buyandelger, W. Linke, P. Zou, S. Kostin, C. Ku, L. Felkin, E. Birks, P. Barton, M. Sattler, R. Knoell, K. Schroder, S. Benkhoff, H. Shimokawa, O. Grisk, R. P. Brandes, I. R. Parepa, L. Mazilu, A. I. Suceveanu, A. Suceveanu, L. Rusali, L. Cojocaru, L. Matei, M. Toringhibel, E. Craiu, A. L. Pires, M. Pinho, S. Pinho, C. Sena, R. Seica, A. Leite-Moreira, F. Dabroi, S. Schiaffino, E. Kiseleva, N. Krukov, O. Nikitin, L. Ardatova, I. Mourouzis, C. Pantos, A. D. Kokkinos, D. V. Cokkinos, E. Scoditti, M. Massaro, M. A. Carluccio, M. Pellegrino, N. Calabriso, A. Gastaldelli, C. Storelli, R. De Caterina, D. Lindner, C. Zietsch, H.-P. Schultheiss, C. Tschope, D. Westermann, B. R. Everaert, V. J. Nijenhuis, F. C. M. Reith, V. Y. Hoymans, J. P. Timmermans, C. J. Vrints, I. Simova, H. Mateev, T. Katova, L. Haralanov, N. Dimitrov, N. Mironov, S. P. Golitsyn, S. F. Sokolov, Y. U. A. Yuricheva, E. B. Maikov, N. B. Shlevkov, L. V. Rosenstraukh, E. I. Chazov, J. Radosinska, V. Knezl, T. Benova, J. Slezak, L. Urban, N. Tribulova, L. Virag, A. Kristof, Z. S. Kohajda, T. Szel, Z. Husti, I. Baczko, N. Jost, A. Varro, A. Sarusi, A. S. Farkas, S. Z. Orosz, T. Forster, A. Farkas, O. M. Zakhrabova-Zwiauer, M. Hardziyenka, R. Nieuwland, H. L. Tan, A. J. A. Raaijmakers, V. J. A. Bourgonje, G. J. M. Kok, A. A. B. Van Veen, M. E. Anderson, M. A. Vos, M. F. A. Bierhuizen, J. Benes, B. Sebestova, I. A. Ghouri, O. J. Kemi, A. Kelly, F. L. Burton, G. L. Smith, S. Ozdemir, K. Acsai, N. Doisne, R. Van Der Nagel, H. D. M. Beekman, T. A. B. Van Veen, K. R. Sipido, G. Antoons, S. C. Harmer, J. S. Mohal, D. Kemp, A. Tinker, D. Beech, D. S. Burley, C. D. Cox, K. T. Wann, G. F. Baxter, R. Wilders, A. Verkerk, P. Fragkiadaki, G. Germanakis, K. Tsarouchas, C. Tsitsimpikou, M. Tsardi, D. George, A. Tsatsakis, P. Rodrigues, C. Barros, A. K. Najmi, V. Khan, M. Akhtar, K. K. Pillai, M. Mujeeb, M. Aqil, C. R. Bayliss, A. E. Messer, M.-C. Leung, D. Ward, J. Van Der Velden, C. Poggesi, C. S. Redwood, S. Marston, A. Vite, E. Gandjbakhch, F. Gary, V. Fressart, P. Leprince, G. Fontaine, M. Komajda, P. Charron, E. Villard, I. Falcao-Pires, C. Gavina, N. Hamdani, G. J. M. Stienen, H. W. M. Niessens, A. F. Leite-Moreira, W. J. Paulus, M. Memo, S. B. Marston, E. Vafiadaki, J. Qian, D. A. Arvanitis, D. Sanoudou, E. G. Kranias, N. Elmstedt, B. Lind, K. Ferm-Widlund, M. Westgren, L.-A. Brodin, C. Mansfield, T. West, M. Ferenczi, P. J. M. Wijnker, D. B. Foster, A. Coulter, A. Frazier, A. M. Murphy, M. Shah, M. B. Sikkel, T. Desplantez, T. P. Collins, P. O' Gara, A. R. Lyon, K. T. Macleod, A. H. Ottesen, W. E. Louch, C. Carlson, O. J. B. Landsverk, M. Stridsberg, I. Sjaastad, E. Oie, T. Omland, G. Christensen, H. Rosjo, J. Cartledge, L. A. Clark, M. Ibrahim, U. Siedlecka, M. Navaratnarajah, M. H. Yacoub, P. Camelliti, C. M. Terracciano, A. Chester, A. Gonzalez-Tendero, I. Torre, F. Garcia-Garcia, J. Dopazo, E. Gratacos, D. Taylor, S. Bhandari, A.-M. Seymour, D. Fliegner, J. Jost, H. Bugger, R. Ventura-Clapier, A. Carpi, M. Campesan, M. Canton, R. Menabo, P. G. Pelicci, M. Giorgio, F. Di Lisa, M. Hancock, A. Venturini, N. Al-Shanti, C. Stewart, R. Ascione, G. Angelini, M.-S. Suleiman, E. Kravchuk, E. Grineva, M. Galagudza, A. Kostareva, A. Bairamov, K. A. Krychtiuk, L. Watzke, C. Kaun, S. Demyanets, J. Pisoni, S. P. Kastl, K. Huber, G. Maurer, J. Wojta, W. S. Speidl, Z. V. Varga, N. Farago, A. Zvara, G. F. Kocsis, M. Pipicz, C. Csonka, T. Csont, G. L. Puskas, P. Ferdinandy, M. Klevstigova, J. Silhavy, D. Manakov, F. Papousek, J. Novotny, M. Pravenec, F. Kolar, O. Novakova, F. Novak, J. Neckar, J. Barallobre-Barreiro, A. Didangelos, X. Yin, M. Fernandez-Caggiano, I. Drozdov, P. Willeit, N. Domenech, M. Mayr, S. Lemoine, S. Allouche, L. Coulbault, P. Galera, J. L. Gerard, J. L. Hanouz, E. Suveren, M. Whiteman, I. M. Studneva, O. Pisarenko, V. Shulzhenko, L. Serebryakova, O. Tskitishvili, A. Timoshin, J. Fauconnier, A. C. Meli, J. Thireau, S. Roberge, A. M. Lompre, E. Jacotot, A. M. Marks, A. Lacampagne, B. Dietel, R. Altendorf, W. G. Daniel, R. Kollmar, C. D. Garlichs, V. Parente, S. Balasso, G. Pompilio, G. Colombo, G. Milano, L. Squadroni, F. Cotelli, O. Pozzoli, M. C. Capogrossi, Y. Ajiro, N. Saegusa, K. Iwade, W. R. Giles, D. M. Stafforini, K. W. Spitzer, R. Sirohi, L. Candilio, G. Babu, N. Roberts, D. Lawrence, A. Sheikh, S. Kolvekar, J. Yap, D. J. Hausenloy, D. M. Yellon, M. Aslam, S. Rohrbach, K.-D. Schlueter, H. M. Piper, T. Noll, D. Guenduez, L. Malinova, V. P. Ryabukho, D. V. Lyakin, T. P. Denisova, S. Montoro-Garcia, E. Shantsila, G. Y. H. Lip, B. Kalaska, E. Sokolowska, K. Kaminski, K. Szczubialka, K. Kramkowski, A. Mogielnicki, M. Nowakowska, W. Buczko, N. Stancheva, E. Mekenyan, K. Gospodinov, S. Tisheva, A. Darago, I. Rutkai, J. Kalasz, A. Czikora, P. Orosz, H. D. Bjornson, I. Edes, Z. Papp, A. Toth, K. Riches, P. Warburton, D. J. O'regan, S. G. Ball, N. A. Turner, I. C. Wood, K. E. Porter, S. Kogaki, H. Ishida, N. Nawa, K. Takahashi, H. Baden, H. Ichimori, T. Uchikawa, S. Mihara, K. Miura, K. Ozono, R. Lugano, T. Padro, M. Garcia-Arguinzonis, L. Badimon, F. Ferraro, R. Viner, J. Ho, D. Cutler, V. Matchkov, C. Aalkjaer, P. A. J. Krijnen, N. E. Hahn, I. Kholova, J. A. Sipkens, F. P. Van Alphen, S. Simsek, C. G. Schalkwijk, J. D. Van Buul, V. W. M. Van Hinsbergh, H. W. M. Niessen, C. G. Caro, A. Seneviratne, C. Monaco, D. Hou, J. Singh, P. Gilson, M. G. Burke, K. B. Heraty, R. Krams, G. Coppola, K. Albrecht, W. Schgoer, D. Wiedemann, N. Bonaros, C. Steger, M. Theurl, U. Stanzl, R. Kirchmair, S. Amadesi, G. Spinetti, E. Cangiano, M. Valgimigli, A. M. Miller, A. Cardinali, K. Vierlinger, G. Pagano, D. Liccardo, C. Zincarelli, G. D. Femminella, A. Lymperopoulos, C. De Lucia, W. J. Koch, D. Leosco, G. Rengo, R. Hinkel, W. Husada, T. Trenkwalder, Q. Di, S. Lee, B. Petersen, I. Bock-Marquette, H. Niemann, M. Di Maio, C. Kupatt, M. Nourian, Z. Yassin, R. Kelishadi, S. H. Memarian, A. Heidari, A. Leuner, D. M. Poitz, C. Brunssen, U. Ravens, R. H. Strasser, H. Morawietz, F. Vogt, A. Grahl, C. Flege, N. Marx, M. Borinski, B. De Geest, F. Jacobs, I. Muthuramu, S. C. Gordts, E. Van Craeyveld, P. Herijgers, S. Weinert, S. Medunjanin, J. Herold, A. Schmeisser, R. C. Braun-Dullaeus, A. H. Wagner, K. Moeller, O. Adolph, M. Schwarz, C. Schwale, C. Bruehl, R. Nobiling, T. Wieland, S. W. Schneider, M. Hecker, A. Cross, A. Strom, J. Cole, M. Goddard, A. Hultgardh-Nilsson, J. Nilsson, C. Mauri, N. P. Mitkovskaya, T. A. Kurak, E. G. Oganova, E. I. Shkrebneva, Z. H. N. Kot, T. V. Statkevich, F. Molica, F. Burger, C. M. Matter, A. Thomas, C. Staub, A. Zimmer, B. Cravatt, P. Pacher, S. Steffens, R. Blanco, R. Sarmiento, C. Parisi, S. Fandino, F. Blanco, G. Gigena, J. Szarfer, A. Rodriguez, A. Garcia Escudero, M. A. Riccitelli, S. Wantha, S. Simsekyilmaz, R. T. Megens, M. A. Van Zandvoort, E. Liehn, A. Zernecke, D. Klee, C. Weber, O. Soehnlein, L. M. Lima, M. G. Carvalho, K. B. Gomes, I. R. Santos, M. O. Sousa, C. A. S. Morais, S. H. V. Oliveira, I. F. Gomes, F. C. Brandao, M. R. A. Lamego, L. Fornai, A. Kiss, F. Giskes, G. Eijkel, M. Fedrigo, M. L. Valente, R. M. A. Heeren, A. Grdinic, D. Vojvodic, N. Djukanovic, A. G. Grdinic, S. Obradovic, I. Majstorovic, S. Rusovic, Z. Vucinic, D. Tavciovski, M. Ostojic, S.-C. Lai, M.-Y. Chen, H.-T. Wu, L. Gouweleeuw, S. U. Oberdorf-Maass, R. A. De Boer, W. H. Van Gilst, A. H. Maass, I. C. Van Gelder, L. Benard, C. Li, D. Warren, C. M. Shanahan, Q. P. Zhang, A. Bye, R. Vettukattil, S. T. Aspenes, G. Giskeodegaard, I. S. Gribbestad, U. Wisloff, T. F. Bathen, J. Cubedo, R. Alonso, P. Mata, I. Ivic, Z. Vamos, P. Cseplo, D. Kosa, O. Torok, J. Hamar, A. Koller, K. Norita, S. V. De Noronha, M. N. Sheppard, I. Amat-Roldan, I. Iruretagoiena, S. Psilodimitrakopoulos, F. Crispi, D. Artigas, P. Loza-Alvarez, J. C. Harrison, S. D. Smart, E. H. Besely, J. R. Kelly, Y. Yao, I. A. Sammut, M. Hoepfner, W. Kuzyniak, E. Sekhosana, B. Hoffmann, C. Litwinski, A. Pries, E. Ermilov, D. Fontoura, A. P. Lourenco, F. Vasques-Novoa, J. P. Pinto, R. Roncon-Albuquerque, I. P. Oyeyipo, L. A. Olatunji, T. O. Usman, V. A. Olatunji, B. Bacova, C. Viczenczova, V. Dosenko, E. Goncalvesova, J. Vanrooyen, S. K. Maulik, S. Seth, A. K. Dinda, A. Jaiswal, G. Mearini, D. Khajetoorians, E. Kraemer, C. Gedicke-Hornung, G. Precigout, T. Eschenhagen, T. Voit, L. Garcia, S. Lorain, P. Mendes-Ferreira, C. Maia-Rocha, R. Adao, R. J. Cerqueira, M. J. Mendes, P. Castro-Chaves, G. W. De Keulenaer, C. Bras-Silva, G. Ruiter, Y. Y. Wong, M. Lubberink, P. Knaapen, P. Raijmakers, A. A. Lammertsma, J. T. Marcus, N. Westerhof, W. J. Van Der Laarse, A. Vonk-Noordegraaf, N. Steinbronn, E. Koch, G. Steiner, A. Berezin, O. A. Lisovaya, A. M. Soldatova, V. A. Kuznetcov, T. N. Yenina, A. Y. U. Rychkov, P. V. Shebeko, R. Altara, M. H. M. Hessel, J. J. R. Hermans, W. M. Blankesteijn, T. A. Berezina, V. Seden, C. Bonanad, J. Nunez, D. Navarro, M. F. Chilet, F. Sanchis, V. Bodi, G. Minana, F. Chaustre, M. J. Forteza, A. Llacer, G. Galasso, N. Ferrara, A. Akhmedov, R. Klingenberg, C. Brokopp, D. Hof, S. Zoller, R. Corti, S. Gay, A. Von Eckardstein, S. P. Hoerstrup, T. F. Luescher, J. Heijman, A. Zaza, D. M. Johnson, Y. Rudy, R. L. M. Peeters, P. G. A. Volders, R. L. Westra, S. Fujita, R. Okamoto, M. Taniguchi, K. Konishi, I. Goto, K. Sugimoto, M. Nakamura, K. Shiraki, C. Buechler, and M. Ito

Subjects
AMP-activated protein kinase, biology, Physiology, Chemistry, Physiology (medical), Mesenchymal stem cell, biology.protein, Cardiology and Cardiovascular Medicine, Cell biology
Published
2012
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14. Seasonal, daily and diel N2 effluxes in permeable carbonate sediments

Author

B. D. Eyre, I. R. Santos, and D. T. Maher

Abstract

Benthic metabolism and inorganic nitrogen and N2 flux rates (denitrification) were measured in permeable carbonate sands from Heron Island (Great Barrier Reef). Some of the N2 flux rates were among the highest measured in sediments. All benthic fluxes showed a significant difference between seasons with higher rates in summer and late summer. There was no distinct response of the benthic system to mass coral spawning. Instead, changes in benthic fluxes over 12 days in summer appears to be driven by tidal changes in water depth and associated changes in phytosynthetically active radiation reaching the sediments. Dark N2 fluxes were strongly correlated to benthic oxygen consumption across all sites and seasons (r2 = 0.64; p < 0.005; slope = 0.036). However, there were seasonal differences with a steeper slope in summer than winter reflecting either more efficient coupling between respiration and nitrification-denitrification at higher temperatures or different sources of organic matter. Adding data from published studies on carbonate sands revealed two slopes in the dark N2 flux versus benthic oxygen consumption relationship. The lower slope (0.035) was most likely due to high carbon : nitrogen (C : N) organic matter from coral reefs, but competition by benthic microalgae for nitrogen, N-fixation or inefficient coupling between respiration and nitrification-denitrification can not be excluded. The steeper slope (0.089) was most likely due to respiration being driven by low C : N phyto-detritus. If the different slopes were driven by the sources of organic matter then global estimates of continental shelf denitrification are probably about right. In contrast, global estimates of continental shelf may be over-estimated if the low slope was due to inefficient coupling between respiration and nitrification-denitrification and also due to reduced N2 effluxes in the light associated with competition by benthic microalgae for nitrogen and N-fixation.

Published
2012
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15. Groundwater and porewater as a major source of alkalinity to a fringing coral reef lagoon (Muri Lagoon, Cook Islands)

Author

T. Cyronak, I. R. Santos, D. V. Erler, and B. D. Eyre

Abstract

To better predict how ocean acidification will affect coral reefs, it is important to understand how biogeochemical cycles on reefs alter carbonate chemistry over various temporal and spatial scales. This study quantifies the contribution of fresh groundwater discharge (as traced by radon) and shallow porewater exchange (as quantified from advective chamber incubations) to total alkalinity (TA) dynamics on a fringing coral reef lagoon along the southern Pacific island of Rarotonga over a tidal and diel cycle. Benthic alkalinity fluxes were affected by the advective circulation of water through permeable sediments, with net daily flux rates of carbonate alkalinity ranging from −1.55 to 7.76 mmol m−2 d−1, depending on the advection rate. Submarine groundwater discharge (SGD) was a source of TA to the lagoon, with the highest flux rates measured at low tide, and an average daily TA flux of 1080 mmol m−2 d−1. Both sources of TA were important on a reef wide basis, although SGD acted solely as a delivery mechanism of TA to the lagoon, while porewater advection was either a sink or source of TA dependant on the time of day. On a daily basis, groundwater can contribute approximately 70% to 80% of the TA taken up by corals within the lagoon. This study describes overlooked sources of TA to coral reef ecosystems that can potentially alter water-column carbonate chemistry. We suggest that porewater and groundwater fluxes of TA should be taken into account in ocean acidification models in order to properly address changing carbonate chemistry within coral reef ecosystems.

Published
2012
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16. The contribution of groundwater discharge to the overall water budget of Boreal lakes in Alberta/Canada estimated from a radon mass balance

Author

A. Schmidt, J. J. Gibson, I. R. Santos, M. Schubert, and K. Tattrie

Abstract

Radon-222, a naturally-occurring radioisotope with a half-life of 3.8 days, was used to estimate groundwater discharge to small lakes in wetland-rich basins in the vicinity of Fort McMurray, Alberta, a region under significant water development pressures including both oil sands mining and in situ extraction. A program of field investigations was carried out in March and July 2008 using a Durridge RAD-7® and RAD Aqua® to measure radon-222 activity distributions in dissolved gas in the water column of two lakes as a tracer of groundwater discharge in the timeframe of 4 half-lives (15 days). Radon activity concentrations in lakes was found to range from 0.5 to 72 Bq/m3, compared to radon activity concentrations in groundwaters, measured using a RAD H2O, in the range of 2000–8000 Bq/m3. Radon mass balance, used in comparison with stable isotope mass balance, suggested that the two lakes under investigation had quite different proportions of annual groundwater inflow, one being close to 0.5% of annual inflow and the other about 14%, with lower values in the former attributed to a larger drainage area/lake area ratio which promotes greater surface connectivity. Interannual variability in groundwater proportions is expected despite constancy of groundwater discharge rates due to observed variability in annual surface runoff. Combination of stable isotope and radon mass balance approaches provides information on flowpath partitioning that is useful for evaluating surface-groundwater connectivity and acid sensitivity of individual water bodies of interest in the Alberta Oil Sands Region.

Published
2009
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17. Factors influencing contralateral lymph node metastasis from oral carcinoma

Author

L P, Kowalski, R, Bagietto, J R, Lara, R L, Santos, E K, Tagawa, and I R, Santos

Subjects
Adult, Aged, 80 and over, Male, Risk Factors, Lymphatic Metastasis, Carcinoma, Squamous Cell, Humans, Neck Dissection, Female, Mouth Neoplasms, Middle Aged, Aged
Abstract

An ipsilateral neck dissection is mandatory during initial treatment stages II-IV oral carcinomas. However, no consensus exists whether or not to perform an elective contralateral neck dissection.Five hundred thirteen consecutive cases of squamous cell carcinoma (269 tongue, 135 floor of the mouth, 44 inferior gingiva, 65 retromolar trigone) were reviewed. Tumor stages were: 69 T1, 227 T2, 217 T3-T4, 263 N0, 250 N1-N3. A total of 563 neck dissections were performed in 448 patients. Univariate and multivariate analysis of risk factors were performed using logistic regression.Two hundred twenty-three patients (49.8%) had positive nodes in the specimen (182 ipsilateral, 36 bilateral, 5 contralateral). Contralateral neck recurrences occurred in 38 cases (33 not submitted to a contralateral neck dissection initially). Multivariate logistic regression analysis demonstrated that clinical stage (p = .0001), tumor crossing midline (p = .0011), and floor of the mouth involvement (p = .0236) were the most important predictors of contralateral metastasis.The contralateral side of the neck is a common and potentially preventable site of recurrence in tumors of the oral cavity. The multivariate model obtained discriminates patients with low and high risk (more than 20%) of contralateral metastasis. The application of this mathematical model can be useful for the indication of contralateral neck dissections, because not all tumors crossing midline are associated to a high risk (stages I and II tumors not involving the floor of the mouth) and not all tumors not crossing midline are at low risk (stages III and IV tumors involving the floor of the mouth).

Published
1999

18. Histochemical study of mucopolysaccharides in epidermal mucous cells and subjacent granular cells of Glossoscolex uruguayensis L. (Righi, 1978)

Author

V D, Dall Pai, I R, Santos Costa, A C, Pacheco, C E, Alves, and N, Macha

Subjects
Mucous Membrane, Epidermal Cells, Histocytochemistry, Animals, Epidermis, Oligochaeta, Glycosaminoglycans
Abstract

Histochemical study of mucopolysaccharides of both mucous secreting and subjacent granular cells of the epidermis of Glossoscolex uruguayensis L (Righi, 1978), has been done. Histochemical tests revealed two major types of mucous cells: large ortochromatic mucous cells and metachromatic mucous cells. The first ones possess alpha-amylase resistant, PAS-positive material, together with little mucic acid, and the latter present a very low rate of neutral mucopolysaccharides and to a variable degree, both carboxylate and sulphate mucopolysaccharides. A third cell type was also detected, presenting a frothy acid like material. Subjacent epidermal granular cells display alpha-amylase resistant, PAS-positive granules, with no acid mucus.

Published
1981

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