Rôle (structure et fonction) des communautés procaryotes (bactéries et archées) dans le cycle de l’azote d’une vasière littorale du Pertuis Charentais : influence des facteurs biotiques et abiotiques par une approche multi-échelle

In diatoms-dominated intertidal mudflats, at low tide the primary production is particularly high and microphytobenthos that can be limited by nitrogen-related nutrients is linked with N-related prokaryotic communities. Thus, this PhD thesis aim at describing by ecological approach, the role of benthic prokaryotic communities especially N-related ones, at various temporal scales linked to microphytobenthos life cycles. Sediment samples from Marennes-Oleron mudflat (Atlantic coast, France) were collected according to 5 layers : 0-0.5 cm, 0.5-1 cm, 1-2 cm, 2-5 cm and 5 to 10 cm below sediment surface (bsf). Various biotic (i.e. chlorophyll a) and abiotic parameters (i.e. nutrients, exopolymeric substances, water content, salinity, pH, temperature…) were recorded and linked with benthic bacterial production, enzymatic activities and N-related functional genes (i.e. implied in nitrification, denitrification, and anammox). Furthermore, the bacterial and archaeal diversity was assessed by 454 pyrosequencing in order to characterize the communities and shift in link with biotic and abiotic drivers. Aiming at evaluating the influence of abiotic parameters and microphytobenthic activities on the prokaryotic communities, in situ measurements were coupled to a semi-controlled approach.Dans les vasières intertidales dominées par les diatomées, la production primaire est particulièrement forte à marée basse. Ce microphytobenthos peut être limité par les nutriments azotés en lien avec les communautés de procaryotes impliquées dans le cycle de l’azote. Ainsi, ce travail de thèse cherche, via une approche écologique, à décrire le rôle des communautés de procaryotes benthiques notamment liées au cycle de l’azote et ce, suivant différentes échelles temporelles liées aux cycles du microphytobenthos. Des échantillons de sédiment ont été prélevés dans la baie de Marennes-Oléron (Côte Atlantique, France) entre 0 et 10 cm de profondeur suivant 5 couches (0-0,5 cm, 0,5-1 cm, 1-2 cm, 2-5 cm, 5-10 cm). Différents facteurs biotiques et abiotiques ont été mesurés et mis en relation avec la production bactérienne, les activités enzymatiques et les gènes fonctionnels liés au cycle de l’azote (impliqués dans la nitrification, la dénitrification et l’anammox). De plus, la diversité bactérienne et archéenne a été évaluée par pyroséquençage 454 afin de caractériser les communautés et leurs dynamiques en lien avec les facteurs forçants biotiques et abiotiques. Dans le but d’évaluer l’influence des paramètres abiotiques et de la production du microphytobenthos, des mesures in situ ont été couplées avec des mesures en conditions semi-contrôlées

Where does the chilean aconcagua river come from? Use of natural tracers for water genesis characterization in glacial and periglacial environments

The Aconcagua river basin (Chile, 32◦S) has suffered the effects of the megadrought over the last decade. The severe snowfall deficiency drastically modified the water supply to the catchment headwaters. Despite the recognized snowmelt contribution to the basin, an unknown streamflow buffering effect is produced by glacial, periglacial and groundwater inputs, especially in dry periods. Hence, each type of water source was characterized and quantified for each season, through the combination of stable isotope and ionic analyses as natural water tracers. The δ18O and electric conductivity were identified as the key parameters for the differentiation of each water source. The use of these parameters in the stable isotope mixing “simmr” model revealed that snowmelt input accounted 52% in spring and only 22–36% during the rest of the year in the headwaters. While glacial supply contributed up to 34%, both groundwater and periglacial exhibited a remarkable contribution around 20% with some seasonal variations. Downstream, glacial contribution averaged 15–20%, groundwater seasonally increased up to 46%, and periglacial input was surprisingly high (i.e., 14–21%). The different water sources contribution quantification over time for the Aconcagua River reported in this work provides key information for water security in this territory.Fil: Crespo, Sebastián Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Pontificia Universidad Católica de Valparaíso; ChileFil: Lavergne, Céline. Universidad de Playa Ancha; ChileFil: Fernandoy, Francisco. Universidad Andrés Bello; ChileFil: Muñoz, Ariel A.. Pontificia Universidad Católica de Valparaíso; ChileFil: Cara Ramirez, Leandro Javier. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Olfos Vargas, Simón. Pontificia Universidad Católica de Valparaíso; Chil

Photoprotective responses of three intertidal Antarctic macroalgae to short-term temperature stress

The Antarctic Peninsula is experiencing one of the highest warming rates globally. In polar regions, macroalgae thrive under extreme environmental conditions, which could worsen because of future climate change scenarios, including increased ultraviolet exposure, extremely low light availability, and fluctuating temperatures, particularly in the intertidal zones. To investigate the potential role of photoprotective and antioxidant mechanisms in response to future increases in sea surface temperatures caused by climate change, we conducted laboratory experiments using three intertidal macroalgae model species: Adenocystis utricularis (Ochrophyta, Phaeophyceae), Pyropia endiviifolia (Rhodophyta, Bangiophyceae), and Monostroma hariotii (Chlorophyta, Ulvophyceae). These algae were collected in Punta Artigas (King George Island, Antarctica) and acclimated at 2°C for 48 h. They were then assessed in laboratory experiments for up to 5 days under two treatments: (1) control conditions at 2°C and (2) elevated tem.perature conditions at 8°C, representing the most negative increment in SSTs estimated by the end of the 21st century. Carbon, nitrogen, pigments (chlorophylls and carotenoids), mycosporine-like amino acids (MAAs), and phenolic compounds were quantified after 3 and 5 days of exposure. For M. hariotii, elevated temperatures led to an increase in the C/N ratio, total antioxidant capacity, and levels of nitrogen, total carotenoids, chlorophyll-a, pigments (chlorophyll-b and violaxanthin), and phenolic compounds. For A. utricularis, elevated temperatures led to elevated C/N ratio and levels of chlorophyll-a and carotenoids (fucoxanthin and β-carotene). For P. endiviifolia, elevated temperatures resulted in elevated levels of carotenoids (lutein and β-carotene), phenolic compounds, and MAAs (porphyra-334, shinorine, and palythine). Thus, our study suggests that increasing water temperatures due to global warming can enhance the photoprotective abilities of three Antarctic intertidal macroalgae (M. hariotii, A. utricularis, and P. endiviifolia), with each species showing specific responses.Financial and logistical support were granted by the Projects INACH N° RG_10_18 and RT_09_16 granted to PC-P and CS, respectively

Desalination effects on macroalgae (part A): Laboratory-controlled experiments with Dictyota spp. from the Pacific Ocean and Mediterranean Sea

Desalination brines from direct seawater intake that get discharged to coastal areas may produce stress responses on benthic marine communities, mostly due to its excess salinity, and especially on sessile organisms; in this context, macroalgae have been understudied in desalination ecotoxicological investigations. In this study, we assessed the short- and long-term cellular tolerance responses in two brown species of the macroalgae genus Dictyota through controlled laboratory conditions. Dictyota kunthii was collected from the eastern Pacific Ocean (average salinity, ~34 psu), whereas Dictyota dichotoma was from the Mediterranean Sea (average salinity, ~37 psu). Each macroalgae species was exposed for up to 7 days to two conditions with increased salinity values: +2 and +7 psu above their natural average salinity. Photosynthetic parameters and oxidative stress measurements were determined. The results showed that, in both Dictyota species, high salinity values induced reduced photoinhibition (Fv/Fm) but increased the primary productivity (ETRmax) and light requirement (EkETR) especially after 7 days. Conversely, the photosynthetic efficiency (αETR) decreased in hypersalinity treatments in D. dichotoma, while there were no changes in D. kunthii. The reactive oxygen species hydrogen peroxide (H2O2) was greater at high salinity values at 3 days for D. dichotoma and after 7 days in D. kunthii, while lipid peroxidation decreases under hypersalinity with time in both species. Despite the evident H2O2 accumulation in both species against hypersalinity, it did not produce oxidative damage and important impairment in the photosynthetic apparatus. These results contribute to understanding the tolerance strategies at the cellular level of Dictyota spp., which may be considered as potential candidates for biomonitoring of desalination impacts in the field.We gratefully thank the financial support from ANID FONDECYT Postdoctoral fellowship #3180394, European Commission Marie Skłodowska-Curie Actions #888415, and ANID INES I+D # INID210013. Financial support for mobility was granted from SEGIB Scholarship and Fundación Carolina of Spain to PM. We also thank TESPOST 04/19 PhD scholarship granted by Universidad de Playa Ancha to PM. The initiative was also funded by Universidad de Playa Ancha through the Concurso Regular de Investigación 2019 no. CEA 19-20

Desalination effects on macroalgae (part b): Transplantation experiments at brine-impacted sites with Dictyota spp. from the Pacific Ocean and Mediterranean Sea

Desalination residual brines are mostly discharged to marine environments, which can produce osmotic stress on sensitive benthic organisms. In this investigation, we performed transplantation experiments nearby desalination plants using two brown macroalgae species from a cosmopolitan genus: Dictyota kunthii (Chile) and Dictyota dichotoma (Spain). Parameters related to photosynthetic activity and oxidative stress were evaluated at 3 and 7 days for D. kunthii, and 3 and 6 days for D. dichotoma; each at 2 different impacted sites and 1 control. We observed that brine exposition at both impacted sites in Chile generated a marked stress response on D. kunthii, reflected in a decrease of primary productivity (ETRmax), light requirement (EkETR), and an excessive thermal dissipation (NPQmax), especially at 7 days. In D. dichotoma, similar impaired photosynthetic activity was recorded but only at the highest brine influence site during day 3. Regarding oxidative stress, both species displayed high levels of H2O2 when exposed to brine-influenced sites. Although in D. kunthii H2O2 content together with lipid peroxidation was higher after 3 days, these returned to baseline values towards day 7; instead, D. dichotoma H2O2 levels increased only at day 6. This easy and practical approach has proven to provide valuable data to address potential impacts of brine discharges at global scale coastal ecosystems.We gratefully thank financial support to ANID FONDECYT Postdoctoral fellowship #3180394, European Commission Marie Skłodowska-Curie Actions #888415, and ANID INES I+D # INID210013. Financial support for mobility granted from SEGIB Scholarship and Fundación Carolina of Spain to PM. Also, we thank TESPOST 04/19 PhD scholarship granted by Universidad de Playa Ancha to PM

Changes in global ocean bottom properties and volume transports in CMIP5 models under climate change scenarios

Changes in bottom temperature, salinity and density in the global ocean by 2100 for CMIP5 climate models are investigated for the climate change scenarios RCP4.5 and RCP8.5. The mean of 24 models shows a decrease in density in all deep basins except the North Atlantic which becomes denser. The individual model responses to climate change forcing are more complex: regarding temperature, the 24 models predict a warming of the bottom layer of the global ocean; in salinity, there is less agreement regarding the sign of the change, especially in the Southern Ocean. The magnitude and equatorward extent of these changes also vary strongly among models. The changes in properties can be linked with changes in the mean transport of key water masses. The Atlantic Meridional Overturning Circulation weakens in most models and is directly linked to changes in bottom density in the North Atlantic. These changes are due to the intrusion of modified Antarctic Bottom Water, made possible by the decrease in North Atlantic Deep Water formation. In the Indian, Pacific and South Atlantic, changes in bottom density are congruent with the weakening in Antarctic Bottom Water transport through these basins. We argue that the greater the 1986-2005 meridional transports, the more changes have propagated equatorwards by 2100. However, strong decreases in density over 100 years of climate change cause a weakening of the transports. The speed at which these property changes reach the deep basins is critical for a correct assessment of the heat storage capacity of the oceans as well as for predictions of future sea level rise

Role (structure and function) of nitrogen-related prokaryotic communities in an intertidal mudflat of the Marennes-Oleron bay : multi-scale influence of biotic and abiotic drivers

Dans les vasières intertidales dominées par les diatomées, la production primaire est particulièrement forte à marée basse. Ce microphytobenthos peut être limité par les nutriments azotés en lien avec les communautés de procaryotes impliquées dans le cycle de l’azote. Ainsi, ce travail de thèse cherche, via une approche écologique, à décrire le rôle des communautés de procaryotes benthiques notamment liées au cycle de l’azote et ce, suivant différentes échelles temporelles liées aux cycles du microphytobenthos. Des échantillons de sédiment ont été prélevés dans la baie de Marennes-Oléron (Côte Atlantique, France) entre 0 et 10 cm de profondeur suivant 5 couches (0-0,5 cm, 0,5-1 cm, 1-2 cm, 2-5 cm, 5-10 cm). Différents facteurs biotiques et abiotiques ont été mesurés et mis en relation avec la production bactérienne, les activités enzymatiques et les gènes fonctionnels liés au cycle de l’azote (impliqués dans la nitrification, la dénitrification et l’anammox). De plus, la diversité bactérienne et archéenne a été évaluée par pyroséquençage 454 afin de caractériser les communautés et leurs dynamiques en lien avec les facteurs forçants biotiques et abiotiques. Dans le but d’évaluer l’influence des paramètres abiotiques et de la production du microphytobenthos, des mesures in situ ont été couplées avec des mesures en conditions semi-contrôlées.In diatoms-dominated intertidal mudflats, at low tide the primary production is particularly high and microphytobenthos that can be limited by nitrogen-related nutrients is linked with N-related prokaryotic communities. Thus, this PhD thesis aim at describing by ecological approach, the role of benthic prokaryotic communities especially N-related ones, at various temporal scales linked to microphytobenthos life cycles. Sediment samples from Marennes-Oleron mudflat (Atlantic coast, France) were collected according to 5 layers : 0-0.5 cm, 0.5-1 cm, 1-2 cm, 2-5 cm and 5 to 10 cm below sediment surface (bsf). Various biotic (i.e. chlorophyll a) and abiotic parameters (i.e. nutrients, exopolymeric substances, water content, salinity, pH, temperature…) were recorded and linked with benthic bacterial production, enzymatic activities and N-related functional genes (i.e. implied in nitrification, denitrification, and anammox). Furthermore, the bacterial and archaeal diversity was assessed by 454 pyrosequencing in order to characterize the communities and shift in link with biotic and abiotic drivers. Aiming at evaluating the influence of abiotic parameters and microphytobenthic activities on the prokaryotic communities, in situ measurements were coupled to a semi-controlled approach