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| 1 | 甘肃宝积山盆地中侏罗世石拐茨康叶表皮构造及古环境意义显示文摘甘肃宝积山盆地中侏罗统窑街组发现茨康类植物化石,通过对其外部形态和表皮构造研究,认定为石拐茨康叶(Czekanowskia(Vachrameevia)shiguaiensis)。对比当前化石及其现存最近对应种(the nearest living equivalent species)—Ginkgo biloba L.的气孔比率,得到宝积山盆地在中侏罗世的古大气CO_2体积分数为1.55×10^(-3),数值接近GEOCARBⅢ碳平衡模型的拟合曲线,表明茨康叶属植物也是恢复古大气CO_2体积分数的良好材料。同时,通过角质层特征进行古环境重建,结果表明宝积山盆地在中侏罗世时期气候较为温和湿润。 | 刘军 马利涛 彭琳 陈应权 张立 范俊杰 闫德飞 | 2016 | 世界地质2016，35，4： | 6 |
| 2 | Geochemistry and Sr-Nd-Pb Isotopes of the Granites from the Hashitu Mo Deposit of Inner Mongolia, China: Constraints on Their Origin and Tectonic Setting显示文摘The Hashitu molybdenum deposit is located in the southern part of the Great Hinggan Range,NE China.Molybdenum mineralization is hosted by and genetically associated with monzogranite and porphyritic syenogranite.Sr-Nd-Pb isotopes of the intrusions show that the porphyritic syenogranite has initial^(87)Sr/^(86)Sr ratios of 0.70418-0.70952,ε_(Nd)(t)values of 1.3 to 2.1(t=143Ma),^(206)Pb/^(204)Pb ratios of 19.191-19.573,^(207)Pb/^(204)Pb ratios of 15.551-15.572,and^(208)Pb/^(204)Pb ratios of38.826-39.143.The monzogranite has initial^(87)Sr/^(86)Sr ratios of 0.70293-0.71305,ε_(Nd)(t)values of 1.1 to2.0(t=147 Ma),^(206)Pb/^(204)Pb ratios of 19.507-20.075,^(207)Pb/^(204)Pb ratios of 15.564-15.596,and^(208)Pb/^(204)Pb ratios of 39.012-39.599.The calculated Nd model ages(T_(DM))for monzogranite and porphyritic syenogranite range from 866 to 1121 Ma and 795 to 1020 Ma,respectively.The granitic rocks in the Hashitu area have the same isotope range as granites in the southern parts of the Great Hinggan Range.The isotope composition indicates that these granites are derived from the partial melting of a juvenile lower crust originating from a depleted mantle with minor contamination by ancient continental crust.The integrating our results with published data and the Late Mesozoic regional tectonic setting of the region suggest that the granites in the Hashitu area formed in an intra-continent extensional setting,and they are related to the thinning of the thickened lithosphere and upwelling of the asthenosphere. | DING Chengwu DAI Pan BAGAS Leon NIE Fengjun JIANG Sihong WEI Junhao DING Chengzhen ZUO Pengfei ZHANG Ke | 2016 | Acta Geologica Sinica(English Edition)2016，90，1： | 3 |
| 3 | An introductory report on the biodiversity of Middle Jurassic Phoenicopsis(Czekanowskiales) from the Ordos Basin, China显示文摘Although the genus Phoenicopsis is the most common member of Czekanowskiales and is considered an indicative representative of the Middle Jurassic Coniopteris–Phoenicopsis assemblage in northern China, little was known about its taxonomy and biodiversity based upon the leaf cuticular structure. In this paper, three subgenera of the genus Phoenicopsis from the Middle Jurassic, Yan'an Formation of the Ordos Basin, China, Phoenicopsis(subg. Phoenicopsis)(Heer) Samylina, P.(subg. Windwardia)(Florin) Samylina and P.(subg. Culgoweria)(Florin) Samylina are identified based upon the leaf epidermal features for the first time. This discovery demonstrates that Phoenicopsis was quite diverse during the Middle Jurassic in northern China. Its biodiversity is significant for further understanding Middle Jurassic paleophytogeography and paleoclimatology of northern China. The current findings show that the three Phoenicopsis subgenera coexisted and flourished in the mixed zone(ecotone) between the Indo-Sinian Floristic Region and the Siberian Floristic Region as seasonal deciduous plants(trees or shrubs) during the Middle Jurassic. They were important elements in the Middle Jurassic deciduous gymnospermous forest community in warm temperate regions with seasonal temperature and precipitation variations. They are interpreted as growing on the hillsides and sloping fields along meandering streams, lakes and swamps in a vast sedimentary basin in a wet and warm environment. | Chunlin Sun Yunfeng Li David L.Dilcher Hongshan Wang Tao Li Yuling Na Anping Wang | 2015 | Science Bulletin2015，60，21： | 1 |
| 4 | 贝加尔茨康叶在新疆白杨河中侏罗统的发现显示文摘茨康类植物是全球中生代植物的重要组成部分,对研究植物界的发展演化具有重要的意义。新疆准噶尔盆地白杨河中侏罗统西山窑组发现茨康类植物化石,通过对其外部形态和表皮构造研究,依据表皮构造下气孔式,脉络区普通表皮细胞5~8列,普通表皮细胞未见中央乳突等特征认定为贝加尔茨康叶—Czekanowskia(Vachrameevia)baikalica。虽然该类植物在中国北方地区含煤地层中分布较多,但茨康叶属(瓦赫拉梅耶夫亚属)过去仅在中国内蒙古自治区石拐盆地中侏罗统有所报道,在新疆地区尚属首次发现。当前材料的研究对了解该属的分类、地理分布及古气候研究等具有一定意义。 | 杨涛 邢梦蝶 白树崇 | 2017 | 沈阳师范大学学报(自然科学版)2017，35，4： | 1 |
| 5 | Insect herbivory immediately before the eclipse of the gymnosperms:The Dawangzhangzi plant assemblage of Northeastern China显示文摘The Early Cretaceous terrestrial revolution involved global shifts from gymnosperm-to angiosperm-dominated floras.However,responses of insect herbivores to these changes remain unexamined.We evaluated 2176 highly sampled plant specimens representing 62 species/morphotypes from the 126 Ma Dawangzhangzi plant assemblage of Northeastern China.Our study consisted of horsetails,ferns,ginkgoaleans,czekanowskialeans,conifers,and an angiosperm.Their herbivory was evaluated by the functional feeding groups of hole feeding,margin feeding,and surface feeding(ectophytic feeders);piercer and suckers,and ovipositing insects(ectoendophytic feeders);mining,galling,and borings(endophytic feeders);and pathogens,collectively constituting 65 damage types(DTs).The plant assemblage was assessed for herbivory richness by DT richness,component community structure,and DT specialization on plant hosts;for herbivory intensity,it was evaluated for DT frequency,herbivorized surface area,and feeding event occurrences.Using feeding event occurrences,the data supported seven species/morphotypes as most intensely herbivorized:Liaoningocladus boii(76.6%),Czekanowskia sp.1(8.4%),Czekanowskia rigida(4.10%),Lindleycladus lanceolatus(3.5%),Ginkgoites sp.2(2.0%),Podozamites sp.1(1.1%),and Solenites sp.1(0.9%).The most herbivorized taxa were pinaleans(conifers),then czekanowskialeans,and lastly ginkgoaleans;the monodominant component community was the conifer Liaoningocladus boii.DT host specialization levels were low.The plant assemblage had an overall low 0.86%of foliage removed by herbivores,explained by physical and chemical antiherbivore defenses,and parasitoid attack.Although Paleozoic,gymnosperm-dominated assemblages had greater herbivory,component community structure of the three most herbivorized taxa are more similar to modern bracken fern and willow than modern gymnosperm taxa. | Lifang Xiao Conrad C.Labandeira Dong Ren | 2022 | Insect Science2022，29，5： | 0 |
| 6 | First report of subgenus Phoenicopsis(Czekanowskiales)from Middle Jurassic of Ordos,China and its paleoclimatic implications显示文摘Subgenus Phoenicopsis( Phoenicopsis) assigned to Czekanowskiales is recognized and a new species,Phoenicopsis( Ph.) ordosensis sp. nov. is first reported from the Middle Jurassic Yan'an Formation of the Ordos Basin,alternate based upon the leaf gross morphology and epidermal structures. The new species has linear leavs in bundles of five to six attached on a short shoot,more than 100 mm long by 5-6 mm wide,containing 10-12 parallel veins at upper portion. The leaf is hypostomatic. Epidermal cells are longitudinally arranged with smooth periclinal wall on the upper cuticle. The narrow non-stomatal zones and wide stomatal zones alternate in the lower cuticle. Stomata in four to five irregular spaced rows are longitudinally oriented in each stomatal zone.Guard cells for each are surrounded by four to five subsidiary cells with undeveloped papillae. Anticlinal walls of ordinary epidermal cells are nearly straight and periclinal walls slightly papillate. The new species shallow stomatal pits kept open and surrounded by unevenly undeveloped bulges. These characters are consistent with those of growth in a humid,rather than an arid climate. The presence of subgenus Phoenicopsis and other taxa of Czekanowskiales in the coal-bearing Yan'an Formation supports the view that the climate in the Ordos Basin was humid and warm with seasonal changes during the Middle Jurassic. | LI Tao LI Yunfeng NA Yuling HUANG Wei TAN Xiao SUN Chunlin | 2015 | Global Geology2015，18，3： | 0 |
| 7 | 宁夏盐池地区宁夏拟刺葵(新种)的首次发现显示文摘宁夏盐池地区中侏罗统延安组井下发现大量茨康类拟刺葵属叶片压型化石,根据其叶部形态学和表皮构造特征建立宁夏拟刺葵(新种)Phoenicopsis(Windwardia)ningxiaensis sp.nov.He。该新种以叶脉稀疏,每枚叶片仅叶脉2~4条,表皮细胞壁直,上表皮气孔带内气孔器单列,下表皮气孔带内气孔器3或4列,上、下表皮普通表皮细胞均无乳突,副卫细胞强烈乳突为特征,区别于属内其他已知各种。当前新种的表皮构造特征反映中侏罗世气候以温暖、潮湿为主。 | 何发岐 杨兵 张新智 黄卓 孙思远 王涛 | 2023 | 世界地质2023，42，3： | 0 |
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