神农架国家级自然保护区沼泽皱蒴藓沼泽特征分析

神农架巴山冷杉采伐迹地第一次发现了沼泽皱蒴藓沼泽，阐述了沼泽皱蒴藓的生物学特征、群落学特征，初步探讨了沼泽形成原因和演替的过程。     

神农架大九湖湿地泥炭藓遗传多样性RAPD研究

泥炭藓是重要的沼泽湿生藓类,其生长情况对环境气候变迁具有直接的指示意义.通过RAPD分子标记对湖北神农架47份泥炭藓样品的遗传多样性进行了研究:(1)对20条随机引物进行筛选,共选出6条重复性好,条带清晰的引物,对47份样品共扩增出40个条带,多态性比率为95%;(2)以遗传相似性系数0.61为界限,可将47份样品划分为4大类群;(3)对泥炭藓扩增条带的聚类分析显示,大九湖湿地泥炭藓遗传多样性与采样点地域之间没有明显的相关性.对上述结果综合分析表明:大九湖湿地泥炭藓遗传多样性水平较低,一定程度上反映出近些年来旅游开发、排水工程改造等人类活动对大九湖湿地自然环境的影响.     

贵州六盘水娘娘山国家湿地公园泥炭藓沼泽金藻孢囊的分类学研究

报道了采自贵州娘娘山国家湿地公园泥炭藓沼泽的金藻孢囊16种，其中5种为中国新记录，2种新形态型.结合扫描电子显微镜（SEM）图对所有的金藻孢囊形态特征和地理分布进行了详细描述，丰富了中国金藻孢囊的生物多样性.     

泥炭沼泽起源及其发育特征的对比研究

通过对白俄罗斯别列金自然保护区与中国东北长白山地区典型泥炭沼泽的考察研究，从泥炭沼泽形成环境和泥炭层特征方面，详细地分析了道莫日里契科，萨弗斯克－莫赫和金川，哈尼四处泥炭沼泽的地形形态，植被类型以及泥炭剖面结构，泥炭类型等的异同性，提出泥炭沼泽形成实质是自然界中物质能量转化过程中的必然产物，也是生物循环与地质循环过程中生物化学作用的结果。     

泥炭沼泽微地貌特征及其形成的水动力机制

草丘微地貌是泥炭沼泽重要的景观特征之一，根据对中国和白俄罗斯不同类型泥炭沼泽的野外观测，分析草丘微地貌的类型，结构和形态，论述了其发育和分布的基本规律，并对草丘微地貌形成的水动力机制做了初步探讨。     

暖地泥炭藓(Sphagnum junhuhnianum)孢子体发育过程观察研究

描述了暖地泥炭藓Sphagnum junhuhnianum孢子体的形态特征及发育过程。实验中统计共474个配子体,其中246个长出孢子体,占配子体总数的51.2%,且配子体多生长1个或3个孢子体。孢子体起初在雌孢叶间呈翠绿色透明状球体,历经黄绿色、淡褐色、褐色、具光泽的深咖啡色球体并开裂,共历时50天。成熟孢蒴的平均直径1.89±0.08 mm,高度2.90±0.08 mm,孢子数量71631±12751个。孢子数量与孢蒴直径和高度相关性显著;蒴柄长度与孢子数量、孢蒴直径和高度相关性不显著。     

中国东北与白俄罗斯泥炭藓泥炭特性的对比研究

以中国东北小兴安岭汤洪岭和白俄罗斯别列金自然保护区的道莫日契科泥炭藓炭为研究对象，通过泥炭剖面特征的分析以及泥炭灰分，ｐＨ、分解度、碳、氮及Ｃ／Ｎ等基本性质的对比，探讨和分析了两地区泥炭藓泥炭理化性质的差异和主要影响因素，并根据我国东北地区泥炭藓泥炭矿层较薄，泥炭储量少的特点，提出对泥炭藓泥炭沼泽进行重点保护的观点。     

建立国际泥炭沼泽资源信息系统

针对当前我国泥炭资源的开发与利用现状，指出建立东北地区与白俄罗斯泥炭资源信息系统的必要性，阐述了建立此系统所具备的条件，系统的设计方案，以及系统的功能特点和应用效果。     

神农架大九湖盆地岩溶塌陷的高分辨率遥感调查

神农架大九湖盆地岩溶塌陷的直径一般在2～20m之间,利用中等分辨率卫星影像很难识别,而通过高分辨率的快鸟（Quickbird）卫星影像,可以容易快速地识别出来,野外实际调查验证显示其识别率相当高,只有一些隐藏在岩壁下的小型落水洞难以在影像上找到．通过影像识别和野外调查,查明了大九湖盆地岩溶塌陷的特征、类型和空间分布规律,为大九湖湿地修复和地质灾害的防治提供了基础资料．     

Spore-pollen-climate factor transfer function and paleoenvironment reconstruction in Dajiuhu, Shennongjia,Central China

The identified results of 121 surface sediment spore-pollen samples in Shennongjia and meteorological data base of 30 years(January,1971―December,2000)of 7 meteorological stations around Dajiuhu, Shennongjia are used in this study.Selecting 55 species of common spore-pollen with the method of space fitting and stepwise regression we construct the pollen climate factor transfer function of annual mean tem- perature:T=7.649-2.33097X Abies -0.10873X Betula -0.17352X Compositae -0.13176X Cruciferae +0.13356XEuphorbiaceae -0.83069X Campanulaceae +1.96494XPyrrosia+0.38411XPteris+2.77741XSelaginella+0.04439XMonolites.We had reconstructed annual mean temperature series by use of the sporo-pollen samples concentra-tion percentage in peat section with 297 cm thickness in Dajiuhu since 15.753 kaBP.The temperature series reflect well the character of climatic change since the late glacial,which indicates extreme cold climate event of the Oldest Dryas,the Older Dryas,the Younger Dryas and the 8.2 kaBP,the same to the climate fluctuations of Bolling Warm Period and Allerod Warm Period,and the character of temperature change fluctuating frequently at the transition age from the late glacial to the Holocene.The reconstructed temperature also indicate Holocene Optimum,late Holocene warm-dry climate,and the character of climatic change in Dajiuhu in the last 1 ka.The conclusion is that the sporo-pollen samples have important climatic significance to surface sediment and the section of Dajiuhu,Shennongjia and important reference value to studying climatic change during the last glaciation by the temperature transfer function and reconstructed temperature series.     

High-resolution geochemistry records of climate changes since late-glacial from Dajiuhu peat in Shennongjia Mountains,Central China

A peat core with depths of 297 cm was obtained from the Dajiuhu Basin(31°29′27″N,109°59′45″E,1760 m)in Hubei Province,Central China.10 AMS ages provide a time control and reveal that this core spans the past about 16.0 kaBP(calibrated age)(1 4C age:13.3 kaBP).Multi-proxy indexes analysis of geochemistry shows the following character of climate and environmental changes since about 16 kaBP:(1) The climate during the late-glacial period was cold and wet as a whole,but fluctuated continually.11.4- 12.6 cal.kaBP,12.6-15.2 cal.kaBP and 15.2-16 kaBP were corresponding respectively to the Younger Drays,Bφlling-Allerφd Warm Period and the Oldest Drays.(2)Inheriting the some climate characteristics of the late-glacial,the climate during the early-Holocene was wet and temperature increased gradually,during which an obvious dry event around 10.6 cal.kaB appeared.(3)The climate during the mid-Holocene was genarally warm and wet.During 9.2-7.5 kaBP,temperature increased gradually, precipitation was less comparatively and the 8.2 kaBP cold event which might be representative in the globe was reflected markedly.Then,multi-proxy records were relatively stable during 6.7-4.2 kaBP, which shows the best water and thermal condition in the Holocene Optimum.(4)Around 4.2 kaBP,the climate and environment transform from warm and wet to cool and dry,which may result in the collapse of the Neolithic Culture and midwifery the civilization of Xia Dynasty in this region.After 0.9 kaBP,the climate turned cool and wet.Climate and environmental changes archived in Dajiuhu peat respond to the global changes since the late-glacial period and can be contrasted to the changes recorded in other high-resolution archives from the East Asia Monsoon region,which take on the variety model that the monsoon strengthened abruptly after the late-glacial,was strong during the early Holocene,subse- quently declined and became weak after the middle Holocene with dry climate.According to our analysis,the driving mechanism should be the response of s     

湖北省苔藓植物资源的研究 I.神农架地区苔藓植物的种类和分布(英文)

报道了位于中国鄂西的神农架地区苔藓植物初步的调查结果．结果表明该地区共有苔藓植物２１６ 种,隶属于 １１４ 属５１ 科． 藓类有１８１ 种,９３ 属,３３ 科,苔类 ３５ 种,２１ 属,１８ 科;其中１２５种是湖北新分布,９ 种为中国特有种     

湖北七姊妹山自然保护区发现亚高山泥炭藓湿地

七姊妹山自然保护区位于湖北省恩施土家族苗族自治州宣恩县的东部,地理位置为109°37′~109°51E′,29°39~′30°5′N,是我国中亚热带向北亚热带的过渡地区[1].2005年6月,我们对七姊妹山自然保护区的自然植被进行考察,在椿木营首次发现了较大面积的亚高山泥炭藓湿地.该湿地位于椿木营的天花板地、落儿坪等地,海拔1 800 m~1 950 m,呈大斑块状分布,总面积约300 hm2.我们在天花板地和落儿坪分别设置了两个20 m×20 m的调查样地,按照B raun-B lan-quet[2]的植被调查方法,对样地内的植物种类,每种植物的优势度与多度、物候期进行了统计.从物种…     

神农架林区河流水文特征初步研究

通过对神农架林区境内四大水系主要河流的河谷形态、水位、流速、降水量、径流量、水质等方面的测量与统计,分析林区四大水系主要河流的水文特征．研究表明：神农架林区境内河流属于高山河流,河流下切强烈,多呈“V”字型狭谷,河宽一般3～10m,河流河谷具有明显幼年期特征．采用单因子指数法分析评价了35条代表性河流水质,以Ⅲ、Ⅳ类水质为主,分别占总调查河流的29％和43％,I、Ⅱ类水质分别占调查河流的3％和11％．各河流水质受单一因子影响十分明显．总体来看,林区河流多数河段受人类活动影响,不同程度地受到了生活污水、工业废水的污染．     

神农架地区米心水青冈群落物种多样性特征

水青冈属(Fagus)植物是北半球温带森林的重要建群种,其中以米心水青冈(Fagus engleriana)分布最为广泛.以湖北神农架为研究点,采用标准样地调查法,应用物种丰富度、Shannon-Wiener指数、Simpson指数、均匀度指数对米心水青冈林群落物种多样性,群落结构特征进行研究.结果表明:乔木层Shannon-Wiener指数为2.55,Simpson指数5.31,均匀度指数0.70,Shannon-Wiener指数与Simpson指数的顺序为草本层＞乔木层＞灌木层.径级分布研究表明整个群落更新状况良好.     

神农架地表水质初步调查分析

介绍2006年7月27日~8月6日对神农架3条河流、2个湿地中的水质分析结果,并参照国家标准,得出了除总磷部分超标以外,其余水体大部分指标符合I类水质标准。分析结果表明,水电站对河流生境破坏程度很大,造成下游削减断面或坝下总磷、COD增大,富营养化趋势加大;梯级开发水电站影响更严重;湿地水质出现富营养化状态。     

Sensitivity of pollen factors in the climate transfer function

Constructing a mathematic transfer function of pollen and climatic factors is one of the most important approaches in the quantitative reconstruction of paleoclimate elements.In the function building,the key point is the response sensitivity to the climate change for different pollen families and categories. As an example in this paper,the pollen samples from the surface and stratum in Dajiuhu basin,Shennongjia are used to estimate the sensitivity of pollen factor-temperature in the transfer function by the EOF analysis,multiple regression and stepwise regression techniques.Thereafter,the selection methods of pollen factors are discussed and compared with other results from different researchers. The results show that in the pollen samples,the quantity of woody plants is larger than others,but the woody plants have relatively lower sensitivity and slow responses to the climate evolution and abrupt climate change.While the pollens from lower grade plants(herb and fern)have a relatively high sensi- tivity to the temperature change and fast response to the abrupt climate changes.Therefore,the pollen of herb and fern may significantly record the extreme events in the climate change.Also in different regions,the pollen samples have different sensitivity and optimum combination in the transfer functions.Final conclusion is that the stepwise regression is one of the best methods for transfer function building since it can obtain the maximum multiple correlation coefficients and optimum combination of sensitive pollen factors.