SHRIMP U-Pb zircon age of tuff at the bottom of the Lower Cambrian Niutitang Formation,Zunyi, South China

A SHRIMP U-Pb zircon geochronology study of the tuff at the bottom of the Lower Cambrian Niutitang Formation at Songlin, Zunyi, South China yielded a mean ^206Pb/^238U age of 518±5 Ma. It is significantly younger than the Re-Os ages of 537--542 Ma for the overlying polymetallic Ni-Mo-PGE-rich layer in the basal Niutitang Formation at Songlin, suggesting that the Re-Os ages might represent that of the original magma chamber for the Ni-Mo-PGE-rich layer rather than the formation age of the strata. The intra-basinal stratigraphic correlation also implies that the absolute age of the Chengjiang biota should be younger than 518±5 Ma. Our new result, together with the SHRIMP U-Pb zircon age for the K-bentonite in the Zhongyicun member of the Zhujiaqing Formation at the Meishucun section, Yunnan Province, provides a temporal constraint for the Lower Cambrian of the Yangtze Platform in South China.     

三水盆地古近纪早期微体生物群及其古环境意义

 对三水盆地SB-01钻孔下古近系地层进行了微体化石分析,共发现介形类7属10种,分布于5个层位;轮藻化石9属15种,见于3个层位。根据介形类和轮藻化石的分布、丰度和分异度变化,讨论了三水盆地古近纪早期的古环境变化。分析结果表明,三水盆地古近纪早期可划分为4个环境演化阶段。阶段A（89.0~75.5 m）：气候较干燥,水体较浅的半咸水环境;阶段B（75.5~53.5 m）：气候温暖潮湿为主,湖平面上升,水体盐度仍较高;阶段C（53.5 ~ 21.0 m）：温湿－干旱气候条件交替出现,湖平面和水体盐度波动频繁;阶段D（21.0 ~ 5.2 m）：气候温暖湿润为主,水体较深,湖水逐渐淡化,相应于湖盆发育盛期。     

配合物[Cu(H2biim)2Cl]ClO4·3H2O的合成和晶体结构

目的以联咪唑、氯化铜及高氯酸为原料合成了新的配合物[Cu（H2biim）2Cl]ClO4.3H2O,并对其结构进行研究。方法以H2biim和CuCl2.2H2O为原料,在水溶液中合成了标题化合物,测定了它的红外紫外光谱和单晶结构。结果X-单晶衍射分析表明该单晶属正交晶系,空间群为Fddd,晶胞参数a=1.217 2（2）nm,b=2.499 8（5）nm,c=2.578 8（5）nm,α=β=γ=90°,V=7.847（3）nm3,Z=16。结论晶体结构分析结果表明,配合物中Cu2＋处于一个畸变的四角锥配位环境,配位原子分别来自联咪唑的4个氮原子和一个氯离子,同时存在丰富的分子内和分子间氢键,构筑了一个三维的超分子体系。     

NaCl胁迫对棉花幼苗生理特性的影响

通过盆栽试验研究了NaCl胁迫对2个不同基因型棉花幼苗叶片叶绿素、可溶性蛋白、丙二醛含量及超氧化物歧化酶、过氧化物酶、过氧化氢酶活性的影响.结果表明:随着NaCl浓度的增加,新陆早13的可溶性蛋白含量显著降低,而赣棉11却显著增加;NaCl胁迫下,二品种棉花的丙二醛含量均有一定增加,但新陆早13的丙二醛含量增加更明显.新陆早13的POD活性随着NaCl浓度的增加显著增加,但赣棉11受NaCl胁迫影响较小.随着NaCl浓度的增加,新陆早13的过氧化氢酶活性显著降低,而赣棉11则显著提高.     

Distribution of ghrelin-like immunoreactive cells in amphioxus, Branchiostoma belcheri – A study of immunohistochemistry

The distribution of ghrelin-like immunoreactive cells in amphioxus (Branchiostoma belcheri) was investigated by using immunohistochemical staining with rabbit antiserum against synthetical mammalian ghrelin. The results showed that ghrelin-like immunoreactive cells were distributed widely in the nervous system, Hatschek’s pit, wheel organ, digestive tract and gonads (ovary and testis). In nervous system, ghrelin-like immunoreactive neurons and their protrusions were distributed speci?cally on the dorsal side, ventral side and funnel part of brain vesicle, with a few dispersive immunoreactive nerve cells and their ?bers in nerve tube. Ghrelin-like immunoreactivities were also detected in Hatschek’s pit epithelial cells and wheel organ cells, with positive substance located along cell membrane. In digestive tract, ghrelin-like immunoreactive cells existed in hepatic diverticulum, anterior and posterior region of midgut, and could be classified into two types, closed- and opened-type endocrine cells. The number of positive cells was most in hepatic diverticulum, secondary in posterior region of midgut and least in anterior region of midgut. In gonads, ghrelin-like immunoreactive substance was detected in oogonia, oocytes and follicle cells in ovary at the small and large growth stages and in early spermatogenic cells and Sertoli cells in testis. The extensive distribution of ghrelin-like cells in amphioxus suggested that these kinds of cells are conservative in evolution and diversified in function. At the same time, we found for the ?rst time that ghrelin-like immunoreactive cells existed in brain vesicle and Hatschek’s pit, which provided new morphological evidence for the existence of an activation pathway between brain vesicle and Hatschek’s pit for the regulation of growth hormone excretion.     

求解对流-扩散方程的一类显示交替分组方法

对求解对流-扩散方程初边值问题的第二类Saul’yev非对称格式以及古典显、隐格式进行组合,提出一种新的求解对流-扩散方程的显示交替分组方法,并对新方法进行稳定性分析和数值实验.新方法针对内点为偶数的情况,在节点两端点处用分组格式进行处理,所得解的精度高,稳定性好,容易在并行机上实现.     

莱阳白垩纪化石生物群

莱阳古生物发现与研究具有辉煌的历史迄今为止,在莱阳地区已经发现3个著名的白垩纪生物群,即早白垩世热河生物群、晚白垩世莱阳恐龙动物群和莱阳恐龙蛋化石群,这在我国乃至世界上其他地方是绝无仅有的。这些化石生物群都集中分布在莱阳五龙河流域,许多重要化石遗址都分布在城郊四周,如金刚口和将军顶等。1923年,我国第一代地质学家谭锡畴在山东莱阳采集了恐     

内蒙古鄂托克旗查布地区恐爪龙类足迹的发现及其意义

内蒙古查布地区下白垩统中保存大量的兽脚类和蜥脚类恐龙足迹以及鸟类足迹化石,2014年再次对内蒙古鄂托克旗野外地质遗迹博物馆(8A和8B化石点)周边的地层进行系统考察,发现两个恐爪龙类恐龙(Deinonychosauria)的二趾型兽脚类足迹,这在鄂托克地区是首次发现。经对比研究,将其归入奔驰龙足迹属(Dromaeosauripus)。与奔驰龙足迹一起发现的还有其他两种兽脚类足迹(Asianopodus robustus和Grallator),反映了恐爪龙类恐龙的生活习性。此类足迹的发现不仅填补了内蒙驰龙足迹(Dromaeopodidae)的空白,增加了世界二趾型足迹的记录,也为鄂托克地区古生态与地层对比提供了素材。     

贵州早二叠世茅口晚期成锰环境及锰矿远景预测

贵州二叠系茅口组中的锰矿有两种类型:一类是茅口组顶部的含锰硅质岩、含锰灰岩和菱锰矿层;另一类是茅口组顶部的含锰岩系经风化淋浊而形成的位于古岩溶侵蚀面之上的遵义式锰矿,含锰岩系为含植物化石、海相化石的粘土岩、含锰粘土岩和菱锰矿层。然而,形成这些锰矿的原生含锰岩系仅分布于台沟相带内,因此,据茅口晚期古地理特征,可分出两个含锰矿带:毕节——仁怀和宣威——遵义含锰矿带;毕节——仁怀和宣威——遵义含锰矿带,其中宣威——遵义含锰矿带可进一步划分出黔北——黔中遵义式锰矿区和黔西原生沉积锰矿区,并提出后者是贵州锰矿勘探的主要目标,特别是在该区寻找含锰岩系古风化面,是寻找具工业意义锰矿的关键。     

早古生代海洋缺氧事件的地质记录与背景机制

早古生代大气氧气含量呈现阶段性上升趋势,在志留纪达到并维持在现代水平(21%),但此期间海洋发生多期次的缺氧事件.尽管这些缺氧事件在规模上无法与中生代的大洋缺氧事件相比,但作为地球系统变化中重要的一环,却对早期海洋生态系统的演化具有重要意义.海洋系统变化研究表明,缺氧事件在形成过程中主要受控于海洋水体循环、营养盐供应、地理地貌条件、气候与海平面变化等因素.不同于中生代的大洋缺氧事件,早古生代海洋生物泵效率增强时,同时还面临大气氧气含量上限变化的影响.衍生于现代缺氧沉积盆地和前寒武纪缺氧海洋模型的水体化学分层理念,对早古生代海洋缺氧事件同样适用.地质记录表明,早寒武世-晚志留世,海洋先后发生8次不同规模的缺氧事件,均可与全球识别的碳同位素漂移对比,并且常常伴随着不同规模的生物灭绝事件.因此,重建缺氧海水的分布范围及氧化还原结构,对研究早古生代海洋生态环境变化具有重要意义.同时,这些事件在纵向上表现出缺氧海底面积占比逐渐缩小的趋势,与同期大气氧气含量的长期爬升、二氧化碳含量的持续降低相吻合.海洋缺氧事件、生物灭绝事件及同期其他构造-气候变化等地质事件,共同构成早古生代地球系统变化的缩影,同...