Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

响应面分析法优化苏云金芽孢杆菌 BRC-ZQL3菌株发酵培养基

从地衣分离获得了Bt菌株BRC-ZQL3,为提高其产孢水平,应用数学统计方法对该菌株发酵培养基进行优化.通过单因子分析,研究碳源、氮源、初始pH等因子对产孢的影响;再采用2水平PlackettBurman设计,筛选影响产孢的8个因子,实验结果表明培养基成分中3个重要影响的因子,分别为CaCO3、玉米粉、酵母膏;利用响应...     

手指口述安全管理方法的探讨

大多数煤矿生产事故是由于人的不安全行为造成的,通过执行"手指口述"方法,可以使员工对自己的操作行为以及作业环境的安全状态进行确认,通过提高员工自主管理和互助保安意识,保证操作过程安全可靠,消除生产事故隐患,从而可以提高安全管理水平,促进矿井安全生产.     

Genome sequence and analysis of the tuber crop potato

Potato (Solanum tuberosum L.) is the world's most important non-grain food crop and is central to global food security. It is clonally propagated, highly heterozygous, autotetraploid, and suffers acute inbreeding depression. Here we use a homozygous doubled-monoploid potato clone to sequence and assemble 86% of the 844-megabase genome. We predict 39,031 protein-coding genes and present evidence for at least two genome duplication events indicative of a palaeopolyploid origin. As the first genome sequence of an asterid, the potato genome reveals 2,642 genes specific to this large angiosperm clade. We also sequenced a heterozygous diploid clone and show that gene presence/absence variants and other potentially deleterious mutations occur frequently and are a likely cause of inbreeding depression. Gene family expansion, tissue-specific expression and recruitment of genes to new pathways contributed to the evolution of tuber development. The potato genome sequence provides a platform for genetic improvement of this vital crop.     

高海拔地区室内富氧浓度安全试验研究

室内富氧可以改善人在高海拔地区的缺氧状况,同时也会带来火灾危险,室内富氧的安全控制已成为重要的研究课题.文章对高海拔地区室内环境富氧条件下滤纸的燃烧速度和安全富氧浓度上限进行了试验研究,并对高海拔地区的富氧安全问题进行了分析.结果表明,在不同海拔地区,室内环境维持相同的氧分压时,滤纸的燃烧速度会随着海拔的升高而显著增加,如果不考虑当地的海拔高度而只以氧分压作为参考会带来火灾危险,但存在富氧的安全氧浓度上限,该氧浓度上限值与环境压力的关系为Y=27.91×exp(-P/44.78)+20.09;海拔不同,富氧到安全氧浓度上限时所对应的相当海拔也不同,该相当海拔与实际海拔的关系为H’=-0.68841+0.63893H+0.0048H2;在海拔高度低于5.55km的地区,通过对室内环境富氧可以安全地将相当海拔降低到3km以下.     

The Effectiveness of Structural Monetary Policy and Macro-Prudential Policies — Based on the DSGE Model That Includes Bank Heterogeneous Credit

Journal of Systems Science and Complexity - Structural monetary policy and macro-prudential policies are important parts of the policy system of the People’s Bank of China. By constructing a...     

弹性半空间-理想流体层中Stoneley波的动力特性

为了解弹性半空一理想流体层中Stoneley波的动力特性,并为进一步开发利用海洋资源提供调查方法,根据弹性固体与理想流体动力学方程,推导了弹性半空间一理想流体层中Stoneley波的特征方程、基于该特征方程,分析了固液两介质的物理特性对流体动压力的影响,以及固体和流体介质的位移分布情况．结果表明,该体系中Stoneley波在固体中的位移分布类似于半空间Rayleigh波,而在流体中的位移分布有明显的规律性;弹性半空一理想流体层中Stoneley波具有频散性,且其波速小于弹性半空间中Rayleigh波的波速．