{"id":"79d259ca-d3ac-458f-ab9e-fe80c3479e39","title":"扎日南木错剖面年代数据","title_en":"Chronological data of mucuo section in zharinan","serial":"","user_limit":"为尊重知识产权、保障数据作者的权益、扩展数据中心的服务、评估数据的应用潜力，请数据使用者在使用数据所产生的研究成果中（包括公开发表的论文、论著、数据产品和未公开发表的研究报告、数据产品等成果），明确注明数据来源和数据作者。对于转载（二次或多次发布）的数据，作者还须注明原始数据来源。","instructions":"文件命名：\n光释光数据命名为：CQ1-A,CQ1-B,CQ1-91,CQ2-26。其中CQ为剖面名字“措勤”首字母，1、2为剖面号，26、A、B为不同深度样品。A、B为1号剖面湖岸堤样品，其余为湖相样品。\n碳十四数据命名为：CQ1-24,CQ1-88B,CQ1-88G。其中CQ为剖面名字“措勤”首字母，1、2为剖面号，24、88为不同深度样品。B、G为不同种类样品，B为大块有机质，G为水生植物残体。\n数据读取方式：\n光释光数据读取方式为：WPS/Office。\n碳十四数据读取方式为：WPS/Office。","description":"青藏高原南部扎日南木错湖一处湖相沉积物剖面的光释光与碳十四年代数据，该数据使用全自动光释光测年仪与加速质谱对样品进行测试，其中光释光实验在中国科学院青海盐湖研究所进行，碳十四测年实验在美国BETA实验室进行。该数据揭示了扎日南木错湖在过去5千年至2千年间的湖泊演化过程。并且，证明了光释光年龄在该处相较碳十四年龄更加合理。除此之外，在研究青藏高原腹地“古泛湖”的演化过程与该区域气候环境变化有着较好的应用价值。","doi":"https://doi.org/10.3389/feart.2021.640172","projection":"","language":"zh","share_type":"online","east":85.9,"west":85.33,"south":30.73,"north":31.08,"scale":null,"crs":null,"filesize":0.01,"share_policy":"a","ts_created":"2021-05-28T10:21:53.953773+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-05-31T10:49:06.081111+08:00","time_description":"5ka-2ka","datas_group":3,"time_description_en":"5ka-2ka","data_format":null,"project":[11],"specials":["b6500306-f60b-4aa1-b0b6-0324d94866df"],"cite":null,"review_status":5,"review_invite":[{"user_name":"李育","username":"李育","email":"liyu@lzu.edu.cn","is_cancel_expert":false}],"review_editor":{"id":42421,"last_login":"2022-04-08T15:16:51.670544+08:00","username":"任慧霞","email":"510727846@qq.com","is_active":true,"is_staff":true,"user_name":"任慧霞"},"data_sources":null,"temporal_resolution":"1000 year < x","spatial_resolution":"10km - 100km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21],"subtopics":{"metadata":"79d259ca-d3ac-458f-ab9e-fe80c3479e39","three_pole":null,"third_pole":null},"username":"陈嵘","review_time":null,"protected_duration":0,"protected_describe":null,"is_important":false,"hit_count":469}