{"id":172,"date":"2019-03-20T22:14:36","date_gmt":"2019-03-20T22:14:36","guid":{"rendered":"https:\/\/cpaleo.uqam.ca\/?page_id=172"},"modified":"2023-05-06T20:31:51","modified_gmt":"2023-05-06T20:31:51","slug":"influence-du-forcage-climatique-holocene-sur-les-dynamiques-ecologiques-hydrologiques-et-du-carbone-de-deux-tourbieres-maritimes-de-lile-danticosti","status":"publish","type":"post","link":"https:\/\/cpaleo.uqam.ca\/en\/influence-du-forcage-climatique-holocene-sur-les-dynamiques-ecologiques-hydrologiques-et-du-carbone-de-deux-tourbieres-maritimes-de-lile-danticosti\/","title":{"rendered":"Influence of Holocene climate forcing on the ecological, hydrological and carbon dynamics of two maritime peatlands on Anticosti Island"},"content":{"rendered":"
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Influence of Holocene climate forcing on the ecological, hydrological and carbon dynamics of two maritime peatlands on Anticosti Island | 2019 \u2013 2021<\/h2>\n\n\n\n
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    Study sites:<\/p>\n\n\n\n

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    • Pluvier<\/li>\n\n\n\n
    • Pointe de l\u2019Est<\/li>\n<\/ul>\n\n\n\n

      Person in charge: Michelle Garneau (UQAM)<\/p>\n\n\n\n

      Graduate student: L\u00e9onie Perrier (M. Sc., UQAM)<\/p>\n<\/div>\n\n\n\n

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      Peatlands are an important component of Anticosti Island's natural landscape, covering approximately 25% of its surface area. Despite their relatively large surface area, the conditions favouring their establishment and development in the regional landscape remain poorly understood. The aim of the project is to reconstruct Holocene ecohydroclimatic conditions and carbon accumulation rates in two maritime peatlands located on the eastern tip of Anticosti Island. Due to Anticosti Island's central position in the Gulf of St. Lawrence, these bogs have developed under the influence of the Gulf's surface conditions, interacting with atmospheric circulation during the Holocene. Peatlands are invaluable paleoenvironmental archives, offering numerous prospects for research into maritime climate.<\/p>\n\n\n\n

      A peat core was collected from the deepest section of each bog to reconstruct the Holocene hydroclimatic conditions of the initiation and development of two maritime bogs located in the eastern part of Anticosti Island. More specifically, the project aims to :<\/p>\n\n\n\n

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      1. Reconstructing ecological and hydrological change over time from assemblages of plant macroremains and thecamoebiens ;<\/li>\n\n\n\n
      2. Quantifying changes in peat and carbon accumulation rates during peatland development;<\/li>\n\n\n\n
      3. Characterize the relationship between regional climatic variability throughout the Holocene and the development of the two maritime peatlands.<\/li>\n<\/ol>\n<\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"

        Influence du for\u00e7age climatique holoc\u00e8ne sur les dynamiques \u00e9cologiques, hydrologiques…<\/p>","protected":false},"author":4,"featured_media":1135,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_kad_post_transparent":"","_kad_post_title":"","_kad_post_layout":"","_kad_post_sidebar_id":"","_kad_post_content_style":"","_kad_post_vertical_padding":"","_kad_post_feature":"","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"_kad_post_classname":"","footnotes":""},"categories":[1],"tags":[29,38,31],"class_list":["post-172","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-carbone","tag-holocene","tag-tourbiere-ombrotrophe"],"_links":{"self":[{"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/posts\/172","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/comments?post=172"}],"version-history":[{"count":12,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/posts\/172\/revisions"}],"predecessor-version":[{"id":1620,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/posts\/172\/revisions\/1620"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/media\/1135"}],"wp:attachment":[{"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/media?parent=172"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/categories?post=172"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cpaleo.uqam.ca\/en\/wp-json\/wp\/v2\/tags?post=172"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}