Bulk properties and isotopic data of sediment cores from the Bounty Trough and Tasman Sea off New Zealand

Glacial/interglacial changes in Southern Ocean's air-sea gas exchange have been considered as important mechanisms contributing to the glacial/interglacial variability in atmospheric CO2. Hence, understanding past variability in Southern Ocean intermediate- to deep-water chemistry and circulation is fundamental to constrain the role of these processes on modulating glacial/interglacial changes in the global carbon cycle. Our study focused on the glacial/interglacial variability in the vertical extent of southwest Pacific Antarctic Intermediate Water (AAIW). We compared carbon and oxygen isotope records from epibenthic foraminifera of sediment cores bathed in modern AAIW and Upper Circumpolar Deep Water (UCDW; 943 - 2066 m water depth) to monitor changes in water mass circulation spanning the past 350,000 years. We propose that pronounced freshwater input by melting sea ice into the glacial AAIW significantly hampered the downward expansion of southwest Pacific AAIW, consistent with climate model results for the Last Glacial Maximum. This process led to a pronounced upward displacement of the AAIW-UCDW interface during colder climate conditions and therefore to an expansion of the glacial carbon pool.

Sea-suface microlayer (SML) and underlying water (ULW) samples focusing on CDOM spectral characteristics during METEOR cruise M91

The coastal upwelling system off the coast of Peru is characterized by high biological activity and a pronounced subsurface oxygen minimum zone, as well as associated emissions of atmospheric trace gases such as N2O, CH4 and CO2. From 3 to 23 December 2012, R/V Meteor (M91) cruise took place in the Peruvian upwelling system between 4.59 and 15.4°S, and 82.0 to 77.5°W. During M91 we investigated the composition of the sea-surface microlayer (SML), the oceanic uppermost boundary directly subject to high solar radiation, often enriched in specific organic compounds of biological origin like chromophoric dissolved organic matter (CDOM) and marine gels. In the SML, the continuous photochemical and microbial recycling of organic matter may strongly influence gas exchange between marine systems and the atmosphere. We analyzed SML and underlying water (ULW) samples at 38 stations focusing on CDOM spectral characteristics as indicator of photochemical and microbial alteration processes. CDOM composition was characterized by spectral slope (S) values and excitation-emission matrix fluorescence (EEMs), which allow us to track changes in molecular weight (MW) of DOM, and to determine potential DOM sources and sinks. Spectral slope S varied between 0.012 to 0.043 1 nm-1 and was quite similar between SML and ULW, with no significant differences between the two compartments. Higher S values were observed in the ULW of the southern stations below 15°S. By EEMs, we identified five fluorescent components (F1-5) of the CDOM pool, of which two had excitation/emission characteristics of amino-acid-like fluorophores (F1, F4) and were highly enriched in the SML, with a median ratio SML : ULW of 1.5 for both fluorophores. In the study region, values for CDOM absorption ranged from 0.07 to 1.47 m-1. CDOM was generally highly concentrated in the SML, with a median enrichment with respect to the ULW of 1.2. CDOM composition and changes in spectral slope properties suggested a local microbial release of DOM directly in the SML as a response to light exposure in this extreme environment. In a conceptual model of the sources and modifications of optically active DOM in the SML and underlying seawater (ULW), we describe processes we think may take place (Fig. 1); the production of CDOM of higher MW by microbial release through growth, exudation and lysis in the euphotic zone, includes the identified fluorophores (F1, F2, F3, F4, F5). Specific amino-acid-like fluorophores (F1, F4) accumulate in the SML with respect to the ULW, as photochemistry may enhance microbial CDOM release by (a) photoprotection mechanisms and (b) cell-lysis processes. Microbial and photochemical degradation are potential sinks of the amino-acid-like fluorophores (F1, F4), and potential sources of reworked and more refractory humic-like components (F2, F3, F5). In the highly productive upwelling region along the Peruvian coast, the interplay of microbial and photochemical processes controls the enrichment of amino-acid-like CDOM in the SML. We discuss potential implications for air-sea gas exchange in this area.

Biogenic composition of the sea-surface microlayer from a mesocosm study (Bergen 2011)

The sea-surface microlayer (SML) is the ocean's uppermost boundary to the atmosphere and in control of climate relevant processes like gas exchange and emission of marine primary organic aerosols (POA). The SML represents a complex surface film including organic components like polysaccharides, pro- teins, and marine gel particles, and harbors diverse microbial communities. Despite the potential relevance of the SML in ocean-atmosphere interactions, still little is known about its structural characteristics and sen- sitivity to a changing environment such as increased oceanic uptake of anthropogenic CO2. Here we report results of a large-scale mesocosm study, indicating that ocean acidification can affect the abundance and activity of microorganisms during phytoplankton blooms, resulting in changes in composition and dynam- ics of organic matter in the SML. Our results reveal a potential coupling between anthropogenic CO2 emis- sions and the biogenic properties of the SML, pointing to a hitherto disregarded feedback process between ocean and atmosphere under climate change.

Upwelling and associated heat flux in the equatorial Atlantic inferred from helium isotope disequilibrium

Sea-to-air and diapycnal fluxes of nitrous oxide (N2O) into the mixed layer were determined during three cruises to the upwelling region off Mauritania. Sea-to-air fluxes as well as diapycnal fluxes were elevated close to the shelf break, but elevated sea-to-air fluxes reached further offshore as a result of the offshore transport of upwelled water masses. To calculate a mixed layer budget for N2O we compared the regionally averaged sea-to-air and diapycnal fluxes and estimated the potential contribution of other processes, such as vertical advection and biological N2O production in the mixed layer. Using common parameterizations for the gas transfer velocity, the comparison of the average sea-toair and diapycnal N2O fluxes indicated that the mean sea-toair flux is about three to four times larger than the diapycnal flux. Neither vertical and horizontal advection nor biological production were found sufficient to close the mixed layer budget. Instead, the sea-to-air flux, calculated using a parameterization that takes into account the attenuating effect of surfactants on gas exchange, is in the same range as the diapycnal flux. From our observations we conclude that common parameterizations for the gas transfer velocity likely overestimate the air-sea gas exchange within highly productive upwelling zones.

Obtención de clones de alcornoque (Quercus suber L.) mediante embriogénesis somática: aplicación de medios líquidos y biorreactores en la sincronización de los procesos de desarrollo y maduración de los embriones

El alcornoque tiene un gran valor ambiental, como integrante de los ecosistemas forestales mediterráneos, e interés comercial por el valor de la bellota (alimentación del cerdo ibérico), el carbón, la madera y sobre todo por las aplicaciones industriales del corcho. Las posibilidades de mejora genética del alcornoque, como las de otras especies forestales, están limitadas por sus largos ciclos reproductivos y porque su propagación vegetativa mediante estaquillado solo es posible en estados muy juveniles. Por ello este sistema de propagación tiene muy poca, o ninguna, utilidad práctica en la mejora genética. La embriogénesis somática es la vía más apropiada para la clonación de muchas especies forestales y ha hecho posible el desarrollo a gran escala de plantaciones multivarietales de coníferas. En alcornoque es posible la regeneración completa de árboles adultos mediante embriogénesis somática. Con los protocolos actuales (en medio semisólido), los embriones se generan formando acúmulos y en la fase de multiplicación conviven embriones en distintos estados de desarrollo. Es un sistema asincrónico, con baja eficacia para la propagación en masa, que no elimina completamente las dificultades para el desarrollo de programas de mejora genética del alcornoque. En otras especies la utilización de medios líquidos ha mejorado: la sincronización, productividad de los cultivos, el manejo y reducido los costes de producción. Por ello el desarrollo de suspensiones embriogénicas de alcornoque se plantea como una vía para aumentar la eficacia de la propagación clonal a gran escala. En la presente tesis se desarrollan cultivos embriogénicos de alcornoque en medio líquido. El capítulo 3 aborda el establecimiento y mantenimiento de suspensiones, el capítulo 4 el desarrollo de una fase de proliferación en medio líquido y el capítulo 5 la utilización de sistemas de cultivo en medio líquido, estacionarios y de inmersión temporal, como vía para favorecer la maduración de los embriones somáticos. Para iniciar los cultivos en medio líquido se emplearon agregados de embriones tomados de la fase de proliferación en medio semisólido. Cuando estos agregados se inocularon directamente en medio líquido no se logró el establecimiento de las suspensiones. El establecimiento se consiguió empleando como inóculo las células y Resumen pequeños agregados embriogénicos, de tamaño comprendido entre 41 y 800 μm, desprendidas por agitación breve de los agregados de embriones. El mantenimiento se logró inoculando en baja densidad masas embriogénicas compactas de tamaño comprendido entre 0,8 y 1,2 mm. Estas suspensiones, muy heterogéneas, mantuvieron su capacidad de proliferación y de regeneración de embriones al menos durante diez subcultivos consecutivos. El protocolo de iniciación y mantenimiento, desarrollado inicialmente con un solo genotipo, fue eficaz cuando se probó sobre otros 11 genotipos de alcornoque. En la fase de proliferación se ensayaron tres tipos de envase y tres velocidades de agitación. La combinación envase × velocidad determinó el intercambio gaseoso, la disponibilidad de oxígeno y el estrés hidrodinámico. Los agregados embriogénicos de alcornoque crecieron incluso en condiciones de hipoxia no siendo la disponibilidad de oxígeno un factor limitante del crecimiento para tasas de trasferencia de oxígeno comprendidas entre 0,11 h-1 y 1,47 h-1. Por otra parte la producción de biomasa creció con el estrés hidrodinámico para valores de índice de cizalladura inferiores a 5 x 10-3 cm min-1. La mayor producción de biomasa se obtuvo con matraces Erlenmeyer de 100 ml y alta velocidad de agitación (160 rpm) mientras que la diferenciación de embriones se vio favorecida por bajas velocidades de agitación (60 rpm) asociadas con bajas disponibilidades de oxígeno. La posibilidad de madurar embriones de alcornoque en medio líquido se estudió utilizando sistemas de inmersión permanente y sistemas de inmersión temporal. En inmersión permanente no se diferenciaron embriones cotiledonares (posiblemente por hiperhidricidad). Los sistemas de inmersión temporal permitieron obtener embriones maduros en estado cotiledonar y capaces de regenerar plantas in vitro. Concentraciones de sacarosa superiores a 60 g l-1 y frecuencias de inmersión iguales o inferiores a una diaria, tuvieron efectos negativos para el desarrollo de los embriones somáticos. En los sistemas de inmersión temporal los parámetros físico-químicos del medio de cultivo se mantuvieron estables y no se observó ninguna limitación de nutrientes. No obstante, estos sistemas se vieron afectados por la evaporación que generó el flujo de aire necesario para desplazar el líquido en cada periodo de inmersión. Abstract ABSTRACT Cork oak is one of the most important tree species of the Mediterranean ecosystem. Besides its high environmental value has a great economic interest due to the sustainable production of acorns (to feed the Iberian pig) charcoal, timber and cork, which is a renewable natural product with various technological applications. As happens with other forest species, cork oak genetic improvement programs are limited by their long life cycles and because vegetative propagation by cuttings it´s only possible in very juvenile plants. Hence this propagation system is useless or has little practical use for breeding cork oak. Plant regeneration by somatic embryogenesis is the most suitable way for cloning many forest species, and it is the enabling technology which has allowed the establishment of large-scale conifer multi-varietal plantations. Clonal plant regeneration of mature cork oak trees can be achieved through somatic embryogenesis. Somatic embryos at different stages of development and forming clusters are produced during the multiplication phase with current protocols (using semisolid medium). This is an asynchronous low-efficient process not suitable for mass propagation, and therefore it does not solve the difficulties presented by cork oak breeding programs. Culture in liquid medium has been used with other species to improve: synchronization, yield, handling, and to reduce production costs. Thus the development of cork oak embryogenic suspension cultures is envisaged as a way to increase the efficiency of large scale clonal propagation. The thesis herein develops cork oak embryogenic cultures in liquid medium. In chapter 3 establishment and maintenance of suspension cultures are developed, chapter 4 studies proliferation phase in liquid medium and chapter 5 considers the use of different systems of culture in liquid medium, both stationary and temporary immersion, as a way to promote somatic embryos maturation. Clusters of embryos taken from proliferating cultures on semisolid medium were used to initiate the cultures in liquid medium. When these clusters were inoculated directly in liquid medium establishment of suspension cultures was not executed. However using, as initial inoculum, cells and cell aggregates with a size between 41 and 800 μm detached from these clusters of embryos, subjected to a brief shaking, suspension cultures could be established. Suspension maintenance was achieved by inoculating compact embryogenic Abstract clumps with a size between 0.8 and 1.2 mm at low density. The suspension cultures, very heterogeneous, retained both their proliferation and embryo regeneration capacity for at least ten consecutive subcultures. The initiation and maintenance protocol, initially developed with a single genotype, was effective when tested on 11 additional genotypes of cork oak. In proliferation phase three types of vessels and three different levels of agitation were assayed. The combination vessel × orbiting speed determined gas exchange, oxygen availability and hydrodynamic stress. Cork oak embryogenic aggregates grew even under hypoxia conditions; oxygen availability at transfer rates between 0.11 and 1.47 h-1 was not a limiting factor for growth. Furthermore the biomass production was increased with hydrodynamic stress when shear rate values were of less than 5 x 10-3 cm min-1. The highest biomass production was obtained with 100 ml Erlenmeyer flask and high stirring speed (160 rpm) while the differentiation of embryos was favored by low agitation speeds (60 rpm) associated with low oxygen availability. The possibility to mature cork oak somatic embryos in liquid medium was studied using both permanent immersion systems and temporary immersion systems. Cotyledonary embryos did not differentiate in permanent immersion conditions (probably due to hyperhydricity). Temporary immersion systems allowed obtaining mature cotyledonary embryos, which were able to regenerate plants in vitro. Sucrose concentrations above 60 g l-1 and immersion frequencies equal to or lower than one each 24 h had negative effects on somatic embryo development. Physicochemical parameters of the culture medium in temporary immersion systems were stable and showed no limitation of nutrients. However, these systems were affected by the evaporation generated by the airflow necessary to relocate the medium at each immersion period.

Evidence for the existence of a sulfonylurea-receptor-like protein in plants: Modulation of stomatal movements and guard cell potassium channels by sulfonylureas and potassium channel openers

Limitation of water loss and control of gas exchange is accomplished in plant leaves via stomatal guard cells. Stomata open in response to light when an increase in guard cell turgor is triggered by ions and water influx across the plasma membrane. Recent evidence demonstrating the existence of ATP-binding cassette proteins in plants led us to analyze the effect of compounds known for their ability to modulate ATP-sensitive potassium channels (K-ATP) in animal cells. By using epidermal strip bioassays and whole-cell patch-clamp experiments with Vicia faba guard cell protoplasts, we describe a pharmacological profile that is specific for the outward K+ channel and very similar to the one described for ATP-sensitive potassium channels in mammalian cells. Tolbutamide and glibenclamide induced stomatal opening in bioassays and in patch-clamp experiments, a specific inhibition of the outward K+ channel by these compounds was observed. Conversely, application of potassium channel openers such as cromakalim or RP49356 triggered stomatal closure. An apparent competition between sulfonylureas and potassium channel openers occurred in bioassays, and outward potassium currents, previously inhibited by glibenclamide, were partially recovered after application of cromakalim. By using an expressed sequence tag clone from an Arabidopsis thaliana homologue of the sulfonylurea receptor, a 7-kb transcript was detected by Northern blot analysis in guard cells and other tissues. Beside the molecular evidence recently obtained for the expression of ATP-binding cassette protein transcripts in plants, these results give pharmacological support to the presence of a sulfonylurea-receptor-like protein in the guard-cell plasma membrane tightly involved in the outward potassium channel regulation during stomatal movements.

Restrictions to Carbon Dioxide Conductance and Photosynthesis in Spinach Leaves Recovering from Salt Stress

Salt accumulation in spinach (Spinacia oleracea L.) leaves first inhibits photosynthesis by decreasing stomatal and mesophyll conductances to CO2 diffusion and then impairs ribulose-1,5-bisphosphate carboxylase/oxygenase (S. Delfine, A. Alvino, M. Zacchini, F. Loreto [1998] Aust J Plant Physiol 25: 395–402). We measured gas exchange and fluorescence in spinach recovering from salt accumulation. When a 21-d salt accumulation was reversed by 2 weeks of salt-free irrigation (rewatering), stomatal and mesophyll conductances and photosynthesis partially recovered. For the first time, to our knowledge, it is shown that a reduction of mesophyll conductance can be reversed and that this may influence photosynthesis. Photosynthesis and conductances did not recover when salt drainage was restricted and Na content in the leaves was greater than 3% of the dry matter. Incomplete recovery of photosynthesis in rewatered and control leaves may be attributed to an age-related reduction of conductances. Biochemical properties were not affected by the 21-d salt accumulation. However, ribulose-1,5-bisphosphate carboxylase/oxygenase activity and content were reduced by a 36- to 50-d salt accumulation. Photochemical efficiency was reduced only in 50-d salt-stressed leaves because of a decrease in the fraction of open photosystem II centers. A reduction in chlorophyll content and an increase in the chlorophyll a/b ratio were observed in 43- and 50-d salt-stressed leaves. Low chlorophyll affects light absorptance but is unlikely to change light partitioning between photosystems.

Ribulose-1,5-Bisphosphate Carboxylase/Oxygenase Content, Assimilatory Charge, and Mesophyll Conductance in Leaves1

The content of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco) (Et; EC 4.1.1.39) measured in different-aged leaves of sunflower (Helianthus annuus) and other plants grown under different light intensities, varied from 2 to 75 μmol active sites m−2. Mesophyll conductance (μ) was measured under 1.5% O2, as well as postillumination CO2 uptake (assimilatory charge, a gas-exchange measure of the ribulose-1,5-bisphosphate pool). The dependence of μ on Et saturated at Et = 30 μmol active sites m−2 and μ = 11 mm s−1 in high-light-grown leaves. In low-light-grown leaves the dependence tended toward saturation at similar Et but reached a μ of only 6 to 8 mm s−1. μ was proportional to the assimilatory charge, with the proportionality constant (specific carboxylation efficiency) between 0.04 and 0.075 μm−1 s−1. Our data show that the saturation of the relationship between Et and μ is caused by three limiting components: (a) the physical diffusion resistance (a minor limitation), (b) less than full activation of Rubisco (related to Rubisco activase and the slower diffusibility of Rubisco at high protein concentrations in the stroma), and (c) chloroplast metabolites, especially 3-phosphoglyceric acid and free inorganic phosphate, which control the reaction kinetics of ribulose-1,5-bisphosphate carboxylation by competitive binding to active sites.

Ozone Sensitivity in Hybrid Poplar Is Correlated with a Lack of Defense-Gene Activation1

Ozone is a major gaseous pollutant thought to contribute to forest decline. Although the physiological and morphological responses of forest trees to ozone have been well characterized, little is known about the molecular basis for these responses. Our studies compared the response to ozone of ozone-sensitive and ozone-tolerant clones of hybrid poplar (Populus maximowizii × Populus trichocarpa) at the physiological and molecular levels. Gas-exchange analyses demonstrated clear differences between the ozone-sensitive clone 388 and the ozone-tolerant clone 245. Although ozone induced a decrease in photosynthetic rate and stomatal conductance in both clones, the magnitude of the decrease in stomatal conductance was significantly greater in the ozone-tolerant clone. RNA-blot analysis established that ozone-induced mRNA levels for phenylalanine ammonia-lyase, O-methyltransferase, a pathogenesis-related protein, and a wound-inducible gene were significantly higher in the ozone-tolerant than in the ozone-sensitive plants. Wound- and pathogen-induced levels of these mRNAs were also higher in the ozone-tolerant compared with the ozone-sensitive plants. The different physiological and molecular responses to ozone exposure exhibited by clones 245 and 388 suggest that ozone tolerance involves the activation of salicylic-acid- and jasmonic-acid-mediated signaling pathways, which may be important in triggering defense responses against oxidative stress.

A GIS-based methodology to quantitatively define an Adjacent Protected Area in a shallow karst cavity: The case of Altamira cave

Different types of land use are usually present in the areas adjacent to many shallow karst cavities. Over time, the increasing amount of potentially harmful matter and energy, of mainly anthropic origin or influence, that reaches the interior of a shallow karst cavity can modify the hypogeal ecosystem and increase the risk of damage to the Palaeolithic rock art often preserved within the cavity. This study proposes a new Protected Area status based on the geological processes that control these matter and energy fluxes into the Altamira cave karst system. Analysis of the geological characteristics of the shallow karst system shows that direct and lateral infiltration, internal water circulation, ventilation, gas exchange and transmission of vibrations are the processes that control these matter and energy fluxes into the cave. This study applies a comprehensive methodological approach based on Geographic Information Systems (GIS) to establish the area of influence of each transfer process. The stratigraphic and structural characteristics of the interior of the cave were determined using 3D Laser Scanning topography combined with classical field work, data gathering, cartography and a porosity–permeability analysis of host rock samples. As a result, it was possible to determine the hydrogeological behavior of the cave. In addition, by mapping and modeling the surface parameters it was possible to identify the main features restricting hydrological behavior and hence direct and lateral infiltration into the cave. These surface parameters included the shape of the drainage network and a geomorphological and structural characterization via digital terrain models. Geological and geomorphological maps and models integrated into the GIS environment defined the areas involved in gas exchange and ventilation processes. Likewise, areas that could potentially transmit vibrations directly into the cave were identified. This study shows that it is possible to define a Protected Area by quantifying the area of influence related to each transfer process. The combined maximum area of influence of all the processes will result in the new Protected Area. This area will thus encompass all the processes that account for most of the matter and energy carried into the cave and will fulfill the criteria used to define the Protected Area. This methodology is based on the spatial quantification of processes and entities of geological origin and can therefore be applied to any shallow karst system that requires protection.

Stable isotope ratios, carbon content and primary production of three sediment cores from the subantarctic eastern Atlantic

We present three new benthic foraminiferal delta13C, delta18O, and total organic carbon time series from the eastern Atlantic sector of the Southern Ocean between 41°S and 47°S. The measured glacial delta13C values belong to the lowest hitherto reported. We demonstrate a coincidence between depleted late Holocene (LH) delta13C values and positions of sites relative to ocean surface productivity. A correction of +0.3 to +0.4 [per mil VPDB] for a productivity-induced depletion of Last Glacial Maximum (LGM) benthic delta13C values of these cores is suggested. The new data are compiled with published data from 13 sediment cores from the eastern Atlantic Ocean between 19°S and 47°S, and the regional deep and bottom water circulation is reconstructed for LH (4-0 ka) and LGM (22-16 ka) times. This extends earlier eastern Atlantic-wide synoptic reconstructions which suffered from the lack of data south of 20°S. A conceptual model of LGM deep-water circulation is discussed that, after correction of southernmost cores below the Antarctic Circumpolar Current (ACC) for a productivity-induced artifact, suggests a reduced formation of both North Atlantic Deep Water in the northern Atlantic and bottom water in the southwestern Weddell Sea. This reduction was compensated for by the formation of deep water in the zone of extended winter sea-ice coverage at the northern rim of the Weddell Sea, where air-sea gas exchange was reduced. This shift from LGM deep-water formation in the region south of the ACC to Holocene bottom water formation in the southwestern Weddell Sea, can explain lower preformed d13CDIC values of glacial circumantarctic deep water of approximately 0.3 per mil to 0.4 per mil. Our reconstruction brings Atlantic and Southern Ocean d13C and Cd/Ca data into better agreement, but is in conflict, however, with a scenario of an essentially unchanged thermohaline deep circulation on a global scale. Benthic delta18O-derived LGM bottom water temperatures, by 1.9°C and 0.3°C lower than during the LH at deepest southern and shallowest northern sites, respectively, agree with the here proposed reconstruction of deep-water circulation in the eastern South Atlantic Ocean.

Blood-respiratory and acid-base changes during extended diving in the bimodally respiring freshwater turtle Rheodytes leukops

Changes in blood-gas, acid-base, and plasma-ion status were investigated in the bimodally respiring turtle, Rheodytes leukops, during prolonged dives of up to 12 h. Given that R. leukops routinely submerges for several hours, the objective of this study was to determine whether voluntarily diving turtles remain aerobic and simultaneously avoid hypercapnic conditions over increasing dive lengths. Blood PO2, PCO2, and pH, as well as plasma concentrations of lactate, glucose, Na+, K+, Cl-, total Ca, and total Mg were determined in venous blood collected from the occipital sinus. Blood PO2 declined significantly with dive length; however, oxy-haemoglobin saturation remained greater than 30% for all R. leukops sampled. No changes were observed in blood PCO2, pH, [HCO3-], or plasma glucose, with increasing dive length. Despite repeated dives lasting more than 2 h, plasma lactate remained less than 3 mmol l(-1) for all R. leukops sampled, indicating the absence of anaerobiosis. Compensatory acid-base adjustments associated with anaerobiosis (e.g. declining [Cl-], increasing total [Ca] and [Mg]) were likewise absent, with plasma-ion concentrations remaining stable with increasing dive length. Results indicate that R. leukops utilises aquatic respiration to remain aerobic during prolonged dives, thus effectively avoiding the development of a metabolic and respiratory acidosis.