2) lake record
湖泊记录
1.
The preliminary study of palaeoclimatic and palaeoenvironmental indicators and their information on geological disasters in lake records;
湖泊记录中的古气候和古环境指标及其地质灾害信息
3) pollen records
孢粉记录
1.
Comprehensive studies on the basis of pollen records from lake cores at 30 sites in the Qinghai_Xizang Plateau have been used to reconstruct temporal_spatial distributions of Holocene vegetations.
青藏高原 30个点湖泊的孢粉记录综合研究显示 :在进入全新世之前 (12kaBP以前 ) ,除最东南部外 ,高原从东到西均发育为荒漠草原植被。
2.
On the basis of pollen records in the lake cores from 30 sites in the Tibetan Plateau, the temporal-spatial distribution of vegetation, climatic changes and the South Asian monsoon development in the plateau in the Holocene are studied.
根据青藏高原 30个点湖泊的孢粉记录综合研究显示 :在进入全新世之前 (12kaBP以前 )除最东南部外 ,高原从东到西均发育为荒漠草原植被 。
3.
The pollen records from Zoige, located in the northeastern Tibetan Plateau, indicate that the climate in this area was unstable during the last 20000 years.
若尔盖黑河牧场ＤＣ剖面的孢粉记录表明，末次冰期晚阶段若尔盖高原的气候表现为不稳定性，即冷暖变化频繁，其基本变化与全球一致。
4) Pollen record
孢粉记录
1.
Based on 14C data and archaeological chronology, pollen records reveal a mixed subtropical evergreen and deciduous broadleaved forest dominated by Quecus and Ulmaceae in the studied area before 5300 cal.
上海广富林地区广富林遗址IT1238和IT0446剖面的孢粉记录,并根据14C数据和遗址层位所建立的年代标尺,通过孢粉分析结果表明,在5300cal。
2.
A new pollen record from the Huguangyan Maar Lake (110°17′E,21°9′N ) in the Leizhou Peninsula, Guangdong Province, China, provides information on vegetation and climate changes since the last glaciation.
通过对湛江湖光岩玛珥湖钻孔孢粉记录的研究认为 ,末次冰期以来 ,该区植被类型从早期的南亚热带季风常绿阔叶林依次演替为 ,中亚热带常绿、落叶阔叶林→南亚热带季风常绿阔叶林→中亚热带常绿 落叶阔叶 针叶混交林 (湖边草地 )→热带季雨林→半常绿季雨林。
3.
The palaeo-vegetation succession and palaeoclimate of Late Pleistocene have been feconstructed from the pollen record of the lake sediments from ancient Heqing Lake.
本文通过鹤庆古湖沉积物的孢粉记录对该区晚更新世的古植被和古气候进行了恢复。
5) sporopollen record
孢粉记录
1.
Origin of the second terraces in the Huangshui drainage area,Qinghai,China,studied based on sporopollen records.;
依据孢粉记录初探青海湟水流域二级阶地的成因
2.
Sporopollen Record in Chuodun Site in Suzhou, Jiangsu and Palaeoenvironment in Taihu Region;
江苏苏州绰墩遗址孢粉记录与太湖地区的古环境
补充资料：巢湖泊山洞景区
泊山洞是形成于２亿４千万年前的古老的石灰岩溶洞，奇景秀色，鬼斧神工，被人们誉为“江淮独秀”。全洞面积约４０００平方米，游程长５００余米，共有三层，分１８大景区，８６个景点，洞道高低起伏，幽邃曲折，时而狭窄崎岖，时而宏大开阔，洞中的钟乳石千姿百态，晶莹剔透，若人物佛像，似飞禽走兽，且洞中有洞、有山、有水，洞内冬暖夏凉，四季如春，进洞游览，可一睹泊山洞大佛、龙王宫、灵霄宝殿、黄姑出嫁、鳄鱼汲水、众仙祝寿、泊山龙潭等名胜，尤其是洞中的石枝、石旗、石花、石鹅管精美绝伦，在我国同类溶洞中实属罕见，洞下层有无底潭，深不可测，其水清甜可口，经专家检验，此水含有丰富的对人体有益的矿物质，是优质天然矿泉水。
洞外的下泊山，苍松如海，翠竹掩映，风景如画。山上慈姑庙相传是为纪念黄巢侄女黄姑而建，香烟缭绕，游人不绝，１９９６年又投资修建“泊山寺”对游人开放，站在下泊山远眺，群山环绕，峰峦叠嶂，田园风光，四时胜景尽收眼底。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条