The role of hypoxia in the regulation of membrane transporters

ATP binding cassette (ABC) and solute carrier (SLC) transporters are responsible for the majority of the transcellular movement of various substrates, including drugs, among epithelial cells. Despite the well characterized regulation of influx (SLC) and efflux (ABC) transporters by endogenous mediators, such as inflammatory cytokines, little is known about how changes in oxygen levels may affect expression of these transporters. In this study we showed that the expression of SLC22A4, SLC22A5, SLC22A1, SLC02B1, SLC10A2, ABCC2 and ABCC3 transporters is upregulated by hypoxia in HT29 colon carcinoma cells, but not in HepG2 hepatocarcinoma cells. Moreover, OCTN1 (SLC22A4), OCT1 (SLC22A1) and OATP-B (SLC02B1) transporter expression is also induced by inflammatory cytokines but in a smaller extent than in hypoxia. Furthermore our experiments indicate that there is no cross talk between HIF-1 and NF-κB pathways in HT-29 cells, but these two pathways act simultaneously activating common genes, such as, some SLC and ABC transporters. Our preliminary results from studies with an in vivo murine model of colitis, suggest that HIF-1is stabilized and OCTN1 is strongly induced during severe inflammation, which can be relevant for a recovery from the inflammatory process. We have also been interested in the distribution of HIF-1α variants among different ethnic groups as well as their contribution for cancer risk. Thus, we have demonstrated that there is an ethnicity-related variation in the frequency of the C1772T (P582S) single nucleotide polymorphism (SNP) in the HIF-1α gene. Furthermore, we performed a case-control study in a breast cancer population and our results suggest that there is no association between this SNP or the rare G1790A (A588T) SNP and the incidence of breast cancer. Taken together, the results obtained in this study contribute to a better knowledge of drug influx and efflux during hypoxia and inflammation as well as to the understanding of the pharmacogenetic variability of the HIF-1.

Optimization of molecular dynamics simulation code and applications to biomolecular systems

Tese de doutoramento, Bioquimica, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2015

Assessing land–ocean connectivity via submarine groundwater discharge (SGD) in the Ria Formosa Lagoon (Portugal): combining radon measurements and stable isotope hydrology

Natural radioactive tracer-based assessments of basin-scale submarine groundwater discharge (SGD) are well developed. However, SGD takes place in different modes and the flow and discharge mechanisms involved occur over a wide range of spatial and temporal scales. Quantifying SGD while discriminating its source functions therefore remains a major challenge. However, correctly identifying both the fluid source and composition is critical. When multiple sources of the tracer of interest are present, failure to adequately discriminate between them leads to inaccurate attribution and the resulting uncertainties will affect the reliability of SGD solute loading estimates. This lack of reliability then extends to the closure of local biogeochemical budgets, confusing measures aiming to mitigate pollution. Here, we report a multi-tracer study to identify the sources of SGD, distinguish its component parts and elucidate the mechanisms of their dispersion throughout the Ria Formosa – a seasonally hypersaline lagoon in Portugal. We combine radon budgets that determine the total SGD (meteoric + recirculated seawater) in the system with stable isotopes in water (δ2H, δ18O), to specifically identify SGD source functions and characterize active hydrological pathways in the catchment. Using this approach, SGD in the Ria Formosa could be separated into two modes, a net meteoric water input and another involving no net water transfer, i.e., originating in lagoon water re-circulated through permeable sediments. The former SGD mode is present occasionally on a multi-annual timescale, while the latter is a dominant feature of the system. In the absence of meteoric SGD inputs, seawater recirculation through beach sediments occurs at a rate of  ∼  1.4  ×  106 m3 day−1. This implies that the entire tidal-averaged volume of the lagoon is filtered through local sandy sediments within 100 days ( ∼  3.5 times a year), driving an estimated nitrogen (N) load of  ∼  350 Ton N yr−1 into the system as NO3−. Land-borne SGD could add a further  ∼  61 Ton N yr−1 to the lagoon. The former source is autochthonous, continuous and responsible for a large fraction (59 %) of the estimated total N inputs into the system via non-point sources, while the latter is an occasional allochthonous source capable of driving new production in the system.