细叶黄芪叶肉原生质体发育早期几种细胞器的变化

在细叶黄芪叶肉原生质体发育早期,细胞器的变化较大。离体培养4h后,线粒体的嵴和基质物质开始增加。培养3—5天后,线粒体的数量增加5倍以上,此时可见大部分线粒体围绕细胞核分布。在培养24h后,高尔基体开始发育,它们主要分布在细胞质周边区域。多糖细胞化学染色表明,高尔基体内沉积着大量嗜银物质。培养1天后,粗面内质网开始发育。培养3天时,部分叶绿体边缘出现一些空隙结构。随着叶绿体内膜结构的消失,淀粉粒增大,叶绿体逐渐转变为造粉质体。     

水淹对钉螺卵影响的透射电镜观察

春汛期钉螺繁殖期在洞庭湖现场进行水淹螺卵试验，观察螺卵结构的动态变化。结果显示，对照组螺卵胶膜由胶原纤维层和基底膜组成，卵细胞核大，呈圆形或椭圆形，染色质丰富，细胞内含丰富线粒体、内质网和分泌颗粒等。水淹１０ｄ时，结构尚未见明显变化；至２０ｄ时，胶膜胶原纤维横纹不清，断裂有空洞，线粒体肿胀，嵴结构不清，核内染色质减少；３０ｄ时，出现核固缩或崩解，线粒体消失。说明在螺卵发育期水淹能很快使其发生病理损     

Conformational Changes Relevant to Channel Activity and Folding within the first Nucleotide Binding Domain of the Cystic Fibrosis Transmembrane Conductance Regulator

Deletion of Phe-508 (F508del) in the first nucleotide binding domain (NBD1) of the cystic fibrosis transmembrane conductance regulator (CFTR) leads to defects in folding and channel gating. NMR data on human F508del NBD1 indicate that an H620Q mutant, shown to increase channel open probability, and the dual corrector/potentiator CFFT-001 similarly disrupt interactions between β-strands S3, S9, and S10 and the C-terminal helices H8 and H9, shifting a preexisting conformational equilibrium from helix to coil. CFFT-001 appears to interact with β-strands S3/S9/S10, consistent with docking simulations. Decreases in T(m) from differential scanning calorimetry with H620Q or CFFT-001 suggest direct compound binding to a less thermostable state of NBD1. We hypothesize that, in full-length CFTR, shifting the conformational equilibrium to reduce H8/H9 interactions with the uniquely conserved strands S9/S10 facilitates release of the regulatory region from the NBD dimerization interface to promote dimerization and thereby increase channel open probability. These studies enabled by our NMR assignments for F508del NBD1 provide a window into the conformational fluctuations within CFTR that may regulate function and contribute to folding energetics.     

A 14C age calibration curve for the last 60 ka: the Greenland-Hulu U/Th timescale and its impact on understanding the Middle to Upper Paleolithic transition in Western Eurasia

This paper combines the data sets available today for ¹⁴C-age calibration of the last 60 ka. By stepwise synchronization of paleoclimate signatures, each of these sets of ¹⁴C-ages is compared with the U/Th-dated Chinese Hulu Cave speleothem records, which shows global paleoclimate change in high temporal resolution. By this synchronization we have established an absolute-dated Greenland-Hulu chronological framework, against which global paleoclimate data can be referenced, extending the ¹⁴C-age calibration curve back to the limits of the radiocarbon method. Based on this new, U/Th-based Greenland_Hulu chronology, we confirm that the radiocarbon timescale underestimates calendar ages by several thousand years during most of Oxygen Isotope Stage 3. Major atmospheric ¹⁴C variations are observed for the period of the Middle to Upper Paleolithic transition, which has significant implications for dating the demise of the last Neandertals. The early part of “the transition” (with ¹⁴C ages > 35.0 ka ¹⁴C BP) coincides with the Laschamp geomagnetic excursion. This period is characterized by highly-elevated atmospheric ¹⁴C levels. The following period ca. 35.0-32.5 ka ¹⁴C BP shows a series of distinct large-scale ¹⁴C age inversions and extended plateaus. In consequence, individual archaeological ¹⁴C dates older than 35.0 ka ¹⁴C BP can be age-calibrated with relatively high precision, while individual dates in the interval 35.0-32.5 ka ¹⁴C BP are subject to large systematic age-‘distortions,’ and chronologies based on large data sets will show apparent age-overlaps of up to ca. 5,000 cal years. Nevertheless, the observed variations in past ¹⁴C levels are not as extreme as previously proposed (“Middle to Upper Paleolithic dating anomaly”), and the new chronological framework leaves ample room for application of radiocarbon dating in the age-range 45.0-25.0 ka ¹⁴C BP at high temporal resolution.     

理化因子导致梅花'南京红'花色色素的颜色变化

梅花是中国的候选国花之一。属于花色苷的梅花'南京红'花色色素用含1％浓盐酸(v／v)的甲醇提取,并呈现纯净的紫红色。体外试验表明:该色素在pH0-3范围内颜色稳定,因不同光质、热、氧化剂、还原剂、螯合剂而呈现无色、墨绿色或黄绿色,因不同金属离子、离子的不同浓度而呈现程度不同的红色、紫色、黑黄色、红中带黑或微蓝绿色,葡萄糖和低浓度苯甲酸钠几乎不影响其色泽,蔗糖使颜色变淡,柠檬酸却使其颜色变深。该文可为梅花红色花色的机理探索、梅花花色苷的分子结构鉴定、梅花红色花色色素的开发利用提供参考和前提。     

长期施磷对黄壤旱地磷库变化及地表径流中磷浓度的影响

对贵州黄壤旱地进行采样以及盆栽试验,探索黄壤旱地磷库的变化及其对地表径流磷量的影响。结果表明,长期施磷后黄壤旱地无机磷占全磷的比例逐渐增高,Al-P、Fc-P和Ca-P积累的顺序为Fe-P>Al-P>Ca-P。长期施磷后黄壤旱地的有效磷和藻类可利用的总磷也不断积累,高磷（Olsen-P>25mg·kg^-1)旱地藻类可利用的总磷与Al-P、Fe-P和Ca-P的相关系数分别为0.859、0.903和0.650,Fc-P对藻类可利用磷量的影响起着最重要的作用。在模拟雨强为63.2mm·h^-1下,降雨30min后,低磷黄壤旱地（Olsen-P为4.62-15.9mg·kg^-1)径流中磷酸根磷含量仅为2.81-4.17μg·L^-1,生物有效性磷含量为0.723-0.876mg·L^-1;高磷黄壤旱地（Olsen-P)为29.4-59.2mg·kg^-1)径流中磷酸根磷含量达到0.026-0.714mg·L^-1,生物有效性磷含量增加到0.996-1.281mg·L^-1;高磷黄壤旱地地表径流磷量能加速水体富营养化的产生。     

江苏海门王浩钻孔全新世钙质超微化石的环境意义

初步研究了海门王浩地区ＷＺＫ０１０、ＷＺＫ２１４、ＷＺＫ３００３钻孔中的全新世钙质超微化石组合,优势种Ｇ．ｏｃｅａｎｉｃａ在组合中平均占９７％,依据化石的种数,丰度和保存状况,自下而上划分３个亚组合,第Ｉ亚组合,深度７４－４７ｍ,由Ｇ．ｏｃｅａｎｉｃａ,Ｈ．ｃａｒｔｅｒｉｉ,Ｈ．ｗａｌｌｉｃｈ ｉｉ,Ｓ．ｌａｍｉｎａ,Ｕ．ｓｉｂｏｇａｅ组成,丰度较高,保存较好,代表前三角洲－浅海环境,第Ⅱ亚组合,     

高压静电场（HVEF）对大豆种子吸胀冷害的影响

高压静电场预处理可不同程度地提高大豆种子抗低温吸胀冷害的能力,处理组种子在低温吸胀时无机离子,可溶性糖和可溶性蛋白的外渗量显著低于对照组,静电场预处理还提高了种子中过氧化氢酶（简ＣＡＴ）、过氧化物酶（简ＰＯＤ）、超氧物歧化酶（简ＳＯＤ）等清除自由基的酶活性,降低了丙二醛（简ＭＤＡ）的积累,促进了种子代谢水平,即提高了种子的淀粉酶、脱氢酶的活力和可溶性蛋白含量,最终提高了发芽率。本文以膜的相变和损伤     

青海湖QH85—14C钻孔孢粉分析及其古气候古环境的初步探讨

本文主要依据青海湖具有~(14)C 年龄数据的 QH 85-14C 钻孔系统孢粉分析资料,将井深4.5m 岩芯所做的孢粉图式从下至上分为五个区域性孢粉带,进而论述了青海湖区11,000年来的植被曾经历了疏林草原(11,000—10,000年 BP)、森林草原(10,000年 BP)、森林(8,000—3,500年 BP)、森林草原(3,500—1,500竿 BP)和疏林草原(1500年前至今),反映的气候序列为凉干→温湿→温干阶段。