Risultati per temperatura (decrease OR increase)~ Mostra 1 - 5 risultati su 5 Laminas_Feed_Writer 2 (https://getlaminas.org) https://info.umar.mx/Search/Results?sort=last_indexed+desc&limit=50&lookfor=temperatura+%28decrease+OR+increase%29%7E&type=AllFields&lng=it 5 0 50 Resposta das algas perifíticas da planície de inundação do alto rio Paraná às alterações de temperatura e ao enriquecimento artificial de nutrientes. Tue, 01 Jan 2008 19:37:55 -0500 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_10121 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_10121 Murakami, Eliza Akane Recurso Open Access 2008 Murakami, Eliza Akane 0 Análisis de las tendencias en temperatura del aire extrema y precipitación diaria en la costa ecuatoriana Fri, 01 Jan 2016 19:37:55 -0500 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_11005 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_11005 Vera, Leonor Recurso Open Access 2016 Vera, Leonor 0 On the climatology, oceanography and fisheries of the Panama Bight Wed, 01 Jan 1969 19:37:55 -0500 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_20924 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_20924 Forsbergh, Eric D. Recurso Open Access 1969 Forsbergh, Eric D. 0 The influence of some environmental variables on the apparent abundance of skipjack tuna, Katsuwonus pelamis, in the Eastern Pacific Ocean Sun, 01 Jan 1989 19:37:55 -0500 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_21216 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_21216 Forsbergh, Eric D. Recurso Open Access 1989 Forsbergh, Eric D. 0 Diferencias en la distribución de merluza (Merluccius hubbsi Marini, 1933) entre otoño y primavera en la Zona Común de Pesca Argentino-Uruguaya. Período 1998-2012 Thu, 01 Jan 2015 19:37:55 -0500 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_8519 https://info.umar.mx/Record/aquadocs_http___hdl_handle_net_1834_8519 Louge, E. Recurso Open Access 2015 Louge, E. 0