Résumé : The mangrove forest is an ecosystem distributed worldwide along tropical andsubtropical coastlines. The environmental conditions are known to affect species distributionpatterns, and to understand them is one of the main goals of biogeography. The association ofenvironmental factors (e.g. temperature and precipitation) and species distribution patterns haschallenged scientists since long. Species are distributed in a geographical space, however, whyspecies are present in a certain location but absent in another is a fundamental question inbiogeography. This PhD thesis aims at better understanding the most intriguing issues relatedto the role of environmental factors associated with mangrove distribution range limits andspecies richness from regional (Brazilian mangroves) to global scales.For the Brazilian mangroves, two scales were used to comprehend the spatial ecological nicheof mangrove tree species. First, the entire Brazilian mangrove-lined coast was considered, andseveral environmental variables were used to explain what is driving mangrove tree speciesdistribution. Second, a detailed analysis of daily Sea Surface Temperature (SST) data for theBrazilian mangrove forest at the southernmost mangrove range limit was done, and comparedwith a site beyond the range limit. The chilling events of SST data, also considering oceancurrents, show that Laguncularia racemosa is probably bounded by the southernmost Brazilianmangrove limit because of a dispersal constraint rather than by the frequency of chillingevents. However, the abundance of L. racemosa in Laguna at the Southern mangrove rangelimit, compared with only a few individuals of A. schaueriana, is probably associated with thechilling events of SST constituting a constraint to the latter species. This proves that mangroverange limits are not explained by a single causeThis PhD thesis also has the objective to evaluate the influence of upwelling intensity onthe distribution worldwide, which is its approach at a global scale. The sea surface temperature(SST) had been identified as one of the key drivers of global mangrove distribution, given thecoincidence of isotherms with mangrove global limits. However, other factors play a role in thevariability of SST. Cold waters from deep ocean layers rise to the surface (upwelling systems),which reduces SST values and can trigger aridity. Although previous research has confirmedthat mangrove distribution is driven by a variety of factors, this PhD thesis additionallydemonstrates a significant influence of upwelling intensity, and hence provides elements for abetter understanding of the factors driving mangrove expansion/retraction at a global scale. Inaddition, this work emphasizes climate and oceanographic processes influencing mangroverange limits. While contributing to a better understanding of some of the most intriguingquestions on the macroecology of mangrove, this PhD thesis also raises new questions thatshould be studied by future research.