中国植被分类系统修订方案

为了推动《中国植被志》研编工作, 该文回顾了中国植被分类系统的发展过程和主要阶段性成果, 提出了作为《中国植被志》研编技术框架组成部分的中国植被分类系统修订方案, 对各植被型组及各植被型进行了简单定义和描述, 并针对中国植被分类系统若干问题, 特别就中国植被分类系统总体框架、混交林的界定以及土壤在植被分类中的重要性等问题进行了讨论。1960年侯学煜在《中国的植被》中首次提出了中国植被分类的原则和系统, 1980年出版的《中国植被》制定了分类等级和划分依据等更加完善的系统, 之后《中国植被及其地理格局——中华人民共和国1:1 000 000植被图说明书》和《中国植物区系与植被地理》以及很多省区的植被专著对该系统进行过修订。2017年宋永昌在《植被生态学》中提出了一个分类等级单位调整的方案。本次提出的中国植被分类系统修订方案基本沿用《中国植被》的植被分类原则、分类单位及系统, 采用“植物群落学-生态学”分类原则, 主要以植物群落特征及其与环境的关系作为分类依据, 包含三级主要分类单位, 即植被型(高级单位)、群系(中级单位)和群丛(低级单位); 在三个主要分类单位之上分别增加辅助单位植被型组、群系组和群丛组, 在植被型和群系之下主要根据群落的生态差异和实际需要可再增加植被亚型或亚群系。修订方案包含了森林、灌丛、草本植被(草地)、荒漠、高山冻原与稀疏植被、沼泽与水生植被(湿地)、农业植被、城市植被和无植被地段9个植被型组, 划分为48个植被型(含30个自然植被型、12个农业植被型、5个城市植被型和无植被地段)。自然植被中有23个植被型进一步划分出了81个植被亚型。     

新元古代大塘坡组黑色页岩中的甲藻甾烷及其生物学意义

大塘坡组黑色页岩为中国扬子地台新元古代间冰期沉积。在湖北长阳古城和湖南花垣民乐的大塘坡组黑色页岩中检测到沟鞭藻的生物标志化合物——甲藻甾烷,这是目前国内地质时代最早的甲藻甾烷的检出报道,结合其它化石资科,表明沟鞭藻与其它真核藻类的系统发生至少在新元古代就已经完成、这与真核生物在新元古代冰期结束前就有很大发展的推测相一致。     

Eviostachya hoegii Stockmans在中国五通组的首次发现

首次描述了Eviostachya hoegii Stockmans的营养部分,通过大量标本的观察,修订了前人有关其生殖部分和解剖部分的描述,并对其生殖部分进行了复原.同意Emberger(1968)的观点,将其归于Eviostachyrales中.     

熊果酸对酒精性骨质疏松大鼠骨形成、骨矿化的影响

目的：探讨熊果酸对酒精所致骨质疏松大鼠骨形成、骨矿化的影响。方法：雄性Wistar大鼠60只,按体重随机分为空白对照 组、熊果酸对照组、模型组、熊果酸低、中、高剂量组,同时分别给予生理盐水、150 mg/kg 熊果酸、50%酒精,50 mg/kg 熊果酸,100 mg/kg 熊果酸,150 mg/kg 熊果酸灌胃。熊果酸对照组生理盐水剂量同空白组,熊果酸低、中、高剂量组酒精剂量同模型组。灌胃共 持续8 周。磷钼酸法检测血清磷(P)含量,比色法检测血清钙(Ca)含量,酶联免疫吸附（ELISA）法检测血清骨钙素(BGP)、骨形成蛋 白-2(BMP-2)浓度;HE 染色法观察股骨结构的病理学变化。结果：与空白对照组相比较,模型组血清BGP、BMP-2 和Ca、P 均明显 降低,且有统计学差异(P < 0.05),但熊果酸对照与空白对照组各项指标结果相近。熊果酸中、高剂量组大鼠血清BGP、Ca 和P 水 平均较模型组有显著升高,差异具有统计学意义(P < 0.05),但仅熊果酸高剂量组血清BMP-2 显著升高(P < 0.05)。股骨组织HE 染色结果显示,空白对照组骨小梁致密、规则且较粗,粗细均匀;模型组骨小梁稀松、不规则、粗细不均匀,甚至可见骨小梁断裂; 熊果酸中、高剂量组骨小梁致密、规则、较厚、粗细均匀,未见骨小梁断裂。结论：熊果酸能够促进酒精性骨质疏松大鼠的骨形成, 抑制骨矿物质的流失,在改善酒精致骨质疏松方面有一定的保护作用。     

Solution Structure of the HIV Protease Inhibitor Acetyl-pepstatin as Determined by NMR and Molecular Modeling

Abstract

The structure of acetyl-pepstatin has been investigated in solution by two-dimensional NMR spectroscopy and molecular modeling. The analysis of DQFCOSY, TOCSY and NOESY spectra lead to a full assignment of the NMR signals both in DMSO-d₆ and in TFE-d₃:H₂O 1:1. Interproton distances, dihedral angles and exchange regimes of NH or OH protons were derived from ROESY connectivities, coupling constants and temperature dependences of the chemical shifts, respectively. Molecular modeling using the NMR distance and dihedral angle constraints obtained in DMSO-d₆ yielded a model showing a well-defined structure for the N-terminal segment Ac-1 to Sta-4, but a flexible structure for the C-terminal segment. The structure was less defined in TFE-d₃:H₂O 1:1 and ¹³C T₁ measurements are indicative of higher mobility. Comparison of the NMR-determined solution structure of acetyl-pepstatin with its crystal structure when bound to HIV-1 protease shows that the conformation is more extended in the complex as a result of intermolecular interactions.     

Taphonomic signatures,ichnofacies analysis and depositional dynamics of fossil macro-invertebrate assemblages of the San Juan Raya Formation,Zapotitlán Basin,Puebla, Mexico

In this paper, we describe the taphofacies and ichnofacies from Aptian strata of the San Juan Raya Formation in the Santa Ana Teloxtoc area, Puebla, Mexico. A composite stratigraphic section was analysed on a bed-by-bed scale up to a total thickness of 765.5 m. Our results show the presence of 10 taphofacies and 3 ichnofacies. The taphofacies and ichnofacies interpretation, and its correlation with the sedimentary lithofacies, enabled the determination of a palaeoenvironmental model for the study area that corresponds to a shallow marine, open-coast, clastic system with episodic sedimentation as a product of storm events. This system had several variations in sub-environments, from foreshore to offshore. Foreshore and shoreface environments are characterised by taphofacies Tf1, Tf2, Tf3 and Tf10 and PsI and SkI ichnofacies, representing lower faunal diversity moments (with the exception of Tf3 taphofacies). Meanwhile, taphofacies Tf4, Tf5, Tf6, Tf7, Tf8 and Tf9 were representative of shelf environments and are described as moments of medium-to-high faunal diversity (with the exception of Tf5 taphofacies).     

共生有生殖器官的Anomozamites的新发现

海房沟异羽叶的新联合(Anomozamites haifanggouensis (Kimura et al.) comb. nov.)是辽西和内蒙古东部中侏罗统海房沟组一种特有的本内苏铁类植物.仅发现一块标本(正、反面印痕).标本上保存3枚营养羽叶,它们同几个苞片状的小叶和一些小孢子叶联合在一起,但球果的雌蕊群部分未被保存.标本被收集于内蒙古东部的宁城县山头乡道虎村附近,产于中侏罗统海房沟组.以往在辽西葫芦岛市的南票和白马石乡上三角城等地的同一层位中也曾发现过很多分散保存的苞片状小叶和相似的小孢子叶.它们最初被潘广(1983)认为是一种双子叶的半被子植物(Cycadicotis),并将小孢子叶视为"具皱纹的雌性种囊".后来,又经Kimura等(1994)详细研究,因未找到任何与被子植物有关的证据,将它们归入一个分类位置不明的形态属Pankuangia,并被描述在P. haifanggouensis种名之下.研究结果表明,本文中被研究的标本是同本内苏铁类的Anomozamites异羽叶相连,从而为这些分散保存的生殖器官的确切分类位置的确定提供了有力的证据.     

A new rhynchonelliform brachiopod Longtancunella with soft-part preservation from the Hongjingshao Formation (Cambrian Stage 3) in Yunnan,South China

Rhynchonelliform brachiopods made their first appearance in early Cambrian, and became a major group within the palaeozoic evolutionary fauna since late Cambrian. Exceptionally preserved fossils from the early Cambrian Lagerstätten provide valuable chances to investigate their phylogeny and ecology. Longtancunella is one of the most interesting early rhynchonelliforms, and has been mainly recovered from the Chengjiang Lagerstätte (Series 2, Stage 3). Here, we report a new rhynchonelliform Longtancunella xiazhuangensis n. sp. from the lower Hongjingshao Formation (upper Stage 3) in Yunnan Province, China. These specimens were well preserved with soft parts, including pinnate mantle canal system and a pedicle. It is identified as a new species based mainly on its difference in shell ornamentations, pinnate mantle canals and pedicle morphology from the type species. Its pedicle looks unusually stout with distinct annulated lamellae on the surface, and reveals crucial evidence in illustrating its ecology and settling strategy as an early marine epifauna. The ecological interaction between L. xiazhuangensis and other marine animals also provides insights into the food web structure in the early Cambrian.     

Fossil liberation: a model to explain high biodiversity in the Triassic Cassian Formation

With 1429 animal species, the Triassic Cassian Formation in the Dolomites, Southern Alps (Italy), yields the highest species richness reported from any spatially constrained pre-Quaternary formation known to science. The high preserved diversity is partly attributable to a high primary diversity governed by the tropical setting, increasing alpha diversity, and the breadth of habitats spurring beta diversity. More important is the excellent preservation of fossils and the ease with which they can be extracted from the poorly lithified sediments. We propose the term ‘liberation Lagerstätten’ to capture this preservational window. In contrast to conservation Lagerstätten, liberation Lagerstätten like the Cassian Formation originate from normal marine conditions but low-grade diagenesis. Molluscs contribute substantially to species richness, comprising 67% of all invertebrate species in the Cassian Formation. The gastropod dominance (39% of all species) is nearly as great as in Recent tropical settings, contradicting the concept of a substantial Cenozoic rise.