between 0 and 45 m deep.” The most extensive meadows are those of Posidonia oceanica , restricted to the Mediterranean coast where this endemic species is slow growing and forms millenary meadows. “The results of this study indicate that it is possible to facilitate the recovery of degraded underwater meadows and the benefits they provide within a few decades through actions that improve environmental conditions and conservation policies” concludes the CSIC researcher at the Institut Mediterrani d’Estudis Avançats, Núria Marbà. In Portugal, the most extensive seagrasses are found in Ria Formosa, Ria de Aveiro and in the Sado, Tejo and Mondego estuaries. Rui Santos explains that “the Portuguese seagrass meadows have been

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severely affected in recent decades, so we must Mongolia Email List increase our efforts to reduce the negative impacts on our meadows. Our study brings optimism, since it shows that the recovery of seagrasses is possible and that interventions in this environment can be successful ”. The study has been carried out thanks to the financing of programs to monitor the state of conservation of European grasslands with local, regional, national and European funds and the European COST Action “Seagrass productivity: from genes to ecosystem management”. The latter has made it possible to share and globally analyze the time series of extension, coverage and abundance of existing seagrass beds in Europe.The loss of ice from glaciers and frozen sheets

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contributes to rising sea levels. But not only that, it also influences ocean circulation, affects the productivity of ecosystems and allows the entry of nutrients into the ocean. These changes are produced by underwater melting and the emergence of icebergs that break off from the end of marine glaciers – whose ice culminates in seawater. In some places, those melting rates of sea glaciers were up to 100 times higher than theory predicted. These glaciers experience ice advance and retreat cycles that may be independent of the climatic situation. However, until now the measurements that existed to know how the submarine ends of these ice masses melted were based on theoretical models, which had never been directly tested before. Now, a team of

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