{"id":1476,"date":"2019-08-25T22:06:04","date_gmt":"2019-08-25T18:06:04","guid":{"rendered":"http:\/\/journal.geonatres.az\/?p=1476"},"modified":"2019-08-25T22:32:07","modified_gmt":"2019-08-25T18:32:07","slug":"az%c9%99rbaycanin-abseron-%c9%99srind%c9%99-paleoekoloji-s%c9%99raitinin-xususiyy%c9%99tl%c9%99ri-v%c9%99-onlarin-rekonstruksiya-metodlari","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/az%c9%99rbaycanin-abseron-%c9%99srind%c9%99-paleoekoloji-s%c9%99raitinin-xususiyy%c9%99tl%c9%99ri-v%c9%99-onlarin-rekonstruksiya-metodlari\/","title":{"rendered":"PECULIARITIES OF PALEOECOLOGICAL CONDITIONS OF ABSHERON\u00a0CENTURY OF AZERBAIJAN AND METHODS OF THEIR RECONSTRUCTION"},"content":{"rendered":"

E.N.Taghiyeva, U.A.Khalilova, A.\u0130.Aliyev, E.V.Muradly<\/strong><\/p>\n

Abstract<\/strong>.\u00a0Paleoecological conditions of Absheron time was characterised more humid and less continental than today. Cold period in early Absheron was replaced by another warm climate, while the average temperature reaches\u00a0 to 14\u00b0C and at the beginning of late Absheron by cooling and by the largest decrease in average annual temperature to\u00a0 12\u00b0C for the whole Absheron time. Dark coniferous formations and broadleaved forests with evergreen elements were widely presented in the composition of vegetation.<\/p>\n

 <\/p>\n

REFERENCES<\/strong><\/p>\n

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    Download the article<\/strong><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

    E.N.Taghiyeva, U.A.Khalilova, A.\u0130.Aliyev, E.V.Muradly Abstract.\u00a0Paleoecological conditions of Absheron time was characterised more humid and less continental than today. Cold period in early Absheron was replaced by another warm climate, while the average temperature reaches\u00a0 to 14\u00b0C and at the beginning of late Absheron by cooling and by the largest decrease in average annual temperature to\u00a0 […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-1476","post","type-post","status-publish","format-standard","hentry","category-mqallr"],"blocksy_meta":[],"yoast_head":"\nPECULIARITIES OF PALEOECOLOGICAL CONDITIONS OF ABSHERON\u00a0CENTURY OF AZERBAIJAN AND METHODS OF THEIR RECONSTRUCTION<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/journal.geonatres.az\/en\/az\u0259rbaycanin-abseron-\u0259srind\u0259-paleoekoloji-s\u0259raitinin-xususiyy\u0259tl\u0259ri-v\u0259-onlarin-rekonstruksiya-metodlari\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:locale:alternate\" content=\"az\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"PECULIARITIES OF PALEOECOLOGICAL CONDITIONS OF ABSHERON\u00a0CENTURY OF AZERBAIJAN AND METHODS OF THEIR RECONSTRUCTION\" \/>\n<meta property=\"og:description\" content=\"E.N.Taghiyeva, U.A.Khalilova, A.\u0130.Aliyev, E.V.Muradly Abstract.\u00a0Paleoecological conditions of Absheron time was characterised more humid and less continental than today. 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