Lipolytic response of ‘diabetic’ mice (db/db) to isoproterenol and propranolol in vivo

Summary The genetically diabetic and obesedb/db mice responded lipolytically to isoproterenol and propranolol similarly to normal mice in vivo. However, considering the large amount of triglyceride in adb/db mouse, we conclude that the in vivo response ofdb/db adipose tissue is deficient in magnitude.     

CENP-E is a putative kinetochore motor that accumulates just before mitosis.

The mechanics of chromosome movement, mitotic spindle assembly and spindle elongation have long been central questions of cell biology. After attachment in prometaphase of a microtubule from one pole, duplicated chromosome pairs travel towards the pole in a rapid but discontinuous motion. This is followed by a slower congression towards the midplate as the chromosome pair orients with each kinetochore attached to the microtubules from the nearest pole. The pairs disjoin at anaphase and translocate to opposite poles and the interpolar distance increases. Here we identify CENP-E as a kinesin-like motor protein (M(r) 312,000) that accumulates in the G2 phase of the cell cycle. CENP-E associates with kinetochores during congression, relocates to the spindle midzone at anaphase, and is quantitatively discarded at the end of the cell division. CENP-E is likely to be one of the motors responsible for mammalian chromosome movement and/or spindle elongation.     

Stimulation of locomotor activity of genetically obese mice by amphetamine

Zusammenfassung Die motorische Aktivität von genetish obesen (ob/ob) und diabetischen (db/db) Mäusen wurde durchd-Amphetamin stärker gesteigert als bei normalen Mäusen, wobei das Regulationszentrum für die motorische Aktivität intakt zu sein scheint.     

高中学生心理压力和体育锻炼调适调查研究

通过对300名高中学生进行的问卷调查结果所做的分析,发现他们普遍存在心理压力的困扰.应全面识别引起高中学生心理压力的压力源,并且控制压力源,提高高中学生适应能力两方面来调适高中学生心理压力.通过比较分析可看出,经常参加体育运动的高中学生,其心理压力困扰的程度明显低于不经常参加者,研究认为,科学锻炼有助于提高高中学生身心健康.     

含氧席夫碱-3d过渡金属配合物的研究(Ⅱ)——2,4-二羟基苯甲醛缩氨基脲及其Ni(Ⅱ)、Zn(Ⅱ)配合物的合成、表征及对超氧自由基抑制实验的研究

本文报导了2,4-二羟基苯甲醛缩氨基脲合Ni(Ⅱ)、Zn(Ⅱ)配合物的合成方法,化合物的化学组成以及配位状态由元素分析,红外光谱,紫外光谱确定。     

Cenozoic stratigraphy of Taiwan: Window into rifting, stratigraphy and paleoceanography of South China Sea

Shallow marine sequences of the northern South China Sea (SCS) are uplifted and exposed by plate convergence in the Taiwan mountain belt. These deposits provide detailed geological information about the rifting event, stratigraphy, sedimentology, paleoclimate and paleoceanography of the shallow SCS to compare with what are recorded in the ODP 1148 deep-sea core. Seismic surveys and marine micropalentological studies show that Eocene sequences in the offshore Taiwan Strait and onland Taiwan mountain belt are all deposited in rifting basins and are covered unconformably by the Late Oligocene-Neogene post-rifting strata. Between syn-rifting and post-rifting sequences, there is a regional break-up unconformity throughout the island. Early Oligocene and Late Eocene strata are missing along the break-up unconformity equivalent to the T7 unconformity in the Pearl River Mouth Basin off south China. This may suggest that the SCS oceanic crust could have initiated between 33 and 39 Ma. Neither obvious stratigraphic gap nor slumping features are found in the Oligocene-Miocene transition interval of Taiwan. This observation highly contrasts with what has been documented from the ODP 1148 deep-sea core. This suggests that the stratigraphic gap and slumping features could only be recorded in the SCS deep sea region, but not in the shallow shelf near Taiwan. Compared to the Middle Miocene paleoceanographic re-organization events in the SCS deep sea, the geological history of the Taiwan shallow sequence shows changes of in sedimentation and faunal composition. Due to the Antarctic glacial expansion at~14 Ma, Middle to late Miocene strata of the Western Foothills show progressive regression sedimentations associated with a decrease of benthic foraminif-eral abundance and a sharp faunal turnover event. Many Early-Middle Miocene endemic benthic foraminifers were extinct in 14-13 Ma and new benthic foraminifers of the Kuroshio Current fauna appeared from 10.2 Ma, comparable with new occurrence of Modern benthic foraminifers at 9 Ma in the Java Sea area. This reveals that the Western Boundary Kuroshio Current in the North Pacific could initiate from 10-9 Ma due to closures of the Indo-Pacific seaways by convergent tectonics between the Australian Continent and the Indonesian Arc in 12-8 Ma. Subduction of the SCS oceanic lithosphere since the Middle Miocene resulted in formation of the Hengchun Ridge accretionary prism and the North Luzon Arc. Occurrence of these two bathymetric highs ( 2400 m) since the Middle Miocene and closures of the inter-arc passages in the North Luzon arc in the last 3.5 Ma would control the water exchanges between the West Pacific and the deep SCS. Accordingly, the tectonic evolution in the Central Range-Hengchun Peninsula accretionary prism and the arc-forearc Coastal Range not only control directly the route for water exchanges between the West Pacific and the SCS, but also indirectly shows a great influence on the geochemistry of deep SCS waters. The latter is best shown by much negative carbon isotope values of benthic foraminifers in the ODP 1148 deep-sea core than the West Pacific records in the last 14 Ma.     

苹果和白梨的属间杂交研究

用杂交种胚离体培养的方法可获得大量的苹果和白梨的属间杂交幼苗。对其进行根尖染色体检查和叶、茎的过氧化物酶同工酶带分析。证实杂交种胚苗是二倍体（２ｎ＝３４），并具有其双亲的基本酶带。