新疆其木干剖面中新世-上新世沉积物粘土矿物特征及其古气候指示意义

为重建新疆其木干地区中新世-上新世古气候,采用X射线衍射、扫描电子显微分析方法,对该区中新世-上新世沉积物中粘土矿物的相对含量、组合类型及显微形貌等进行了研究。结果显示:中新世早期-早中新世中期,沉积物中粘土矿物以伊利石和绿泥石为主,含少量的蒙脱石,表明以干旱气候为特征;晚中新世中期-早中新世晚期,伊利石的相对含量逐渐降低,且含有少量的蒙脱石和高岭石,指示相对温湿的气候条件;中新世晚期的粘土矿物组分与中新世早期相似,以伊利石和绿泥石为主,指示古气候以干旱为主导;晚中新世晚期至上新世伊利石相对含量降低,而蒙脱石和高岭石的相对含量升高,但由于粘土矿物中伊利石、绿泥石的含量仍然较高,指示古气候仍然以干旱为主导,但相对于中新世而言,这段时期为相对湿润期。以上结果表明,新疆其木干地区中新世-上新世古气候以干旱为主,并且气候经历了干旱-相对湿润-干旱-相对湿润的演化过程,但总体而言,本区中新世比上新世要更为干旱。     

桂西南岩溶区八种适生植物光合性状的变异与关联

为探究岩溶植物的光合生理适应机制，采用Li-6400XT便携式光合作用测量系统，对广西平果市岩溶区8种适生植物的叶片净光合速率(P_n)、气孔导度(G_s)、胞间CO₂浓度(C_i)、蒸腾速率(T_r)、水分利用效率(WUE)和气孔限制值(L_s)等光合特征参数进行了测定分析。结果表明：(1)6个光合特征参数在种内和种间均存在不同程度的变异，并且种内变异均大于种间变异。(2)G_s和T_r的变化主要来源于种间变异(46.72%～49.76%),而P_n、C_i、WUE和L_s变化主要来源于种内变异(48.66%～64.50%)。在生活型水平上，P_n、G_s和T_r的种内变异表现为常绿植物小于落叶植物，而C_i、WUE和L_s则相反。(3)各参数的种间变异均表现为落叶植...     

Phylogenetic origin of <Emphasis Type="Italic">Salmo trutta</Emphasis> L 1758 from Sicily,based on mitochondrial and nuclear DNA analyses

The phylogenetic status of brown trout Salmo trutta L 1758 in Sicily is uncertain as some reports describe these trout as S. macrostigma or S. cettii on one hand while other, contradictory reports imply a hatchery origin on the other. In order to clarify this situation, we performed sequence analysis of the mtDNA control region and restriction fragment analysis of the nuclear lactate dehydrogenase (LDH-C1*) gene. A single mitochondrial haplotype (At-s6) found previously in brown trout in Morocco, and two alleles at LDH-C1* (the ancestral*100, at a high frequency, and *90) were revealed. Our results suggest that Sicilian brown trout are native and that they probably colonized Sicily from west to east in an expansion, from the Atlantic Ocean basin, along the North-West African coast. Handling editor: C. Sturmbauer     

西南岩溶地区黄荆和檵木叶片结构对其生态环境的响应

应用常规石蜡切片法对生长于桂林毛村岩溶区和非岩溶区的黄荆(Vitex negundo)和檵木(Loropetalumchinense)的解剖特征进行了比较研究,并对两区的黄荆叶片表皮形态进行了扫描电镜观察.结果显示:(1)两地的黄荆叶片背面均有浓密的绒毛,但致密程度有差异,岩溶区黄荆叶片的气孔深藏于绒毛间隙,这种结构可减少水分蒸发,降低因岩溶干旱带来的水分缺失.(2)岩溶区黄荆和檵木的叶片厚度、上下表皮厚度、栅栏组织的厚度以及栅栏组织的致密程度均大于非岩溶区,这些特征有利于减少水分蒸腾.(3)岩溶区黄荆和檵木叶片的维管组织发达程度高于非岩溶区,有利于在蒸腾减小的情况下促进水分运输和营养元素的迁移,说明2种植物叶片结构特征在不同生境区的改变是其长期在岩溶区干旱环境条件下形成的适应性变化.     

不同季节高原鼢鼠乳酸脱氢酶活力和同工酶谱

目的:探讨高原鼢鼠对洞道低氧高二氧化碳环境的代谢适应机制。方法:用酶活力分析法,分析春季、夏季和秋季高原鼢鼠血清乳酸脱氢酶(LDH)活力、乳酸含量和组织LDH活力,用聚丙烯酰胺凝胶电泳法分析血清和组织LDH同工酶谱。结果:高原鼢鼠血清LDH活力在春夏秋三季具有明显的差异,春季高于夏季,夏季高于秋季,血清乳酸含量表现出同样的变化趋势;春季血清中五种同工酶条带都清晰可见,夏季血清中LDH5和LDH4清晰可见,秋季血清中只能看见LDH5带。骨骼肌、心肌和脑组织LDH活力较高,而且从春季到秋季显著降低;肝、肾和肺组织LDH活力较低,肝组织LDH活力春季显著高于夏季和秋季,夏秋两季之间没有明显差异;肾和肺组织LDH活力在春季与夏季之间没有明显差异,但秋季明显降低。心、肝、肺、肾、脑和肌肉组织LDH同工酶谱,在春夏秋三季都显示出五条带,并表现出明显的组织差异;各组织同工酶含量也有不同程度的季节差异。结论:高原鼢鼠体内糖酵解过程具有明显的季节性变化,从春季到秋季依次降低,这与它们的季节性活动特点和洞道中氧气和二氧化碳的季节性波动有关。     

Effect of imitated global warming on Δ<Superscript>13</Superscript>C values in seven plant species growing in tibet alpine meadows

Open-top chambers were used to estimate the possible effects of global warming on δ¹³C of seven plant species grown in alpine meadow ecosystem. The δ¹³C values of plant species were lower after long-term growth in open-top chambers. In the course of experiment, temperature significantly increased inside the chambers by 4°C. Plant species grown at a lower elevation above sea level had higher δ¹³C values as compared to those grown at a higher elevation. This was in accordance with the effect of open-top chamber on δ¹³C values in plants. Greater availability of CO₂ and lower water vapor pressure at higher temperature inside the chambers, as indicated by an increase in discrimination against ¹³CO₂, probably result in more negative δ¹³C values of plants because higher stomatal conductance increases availability of CO₂ and causes greater discrimination against ¹³CO₂. The plant species studied could be the indicator species for testing global warming by the change in carbon isotope ratios at the two growth temperatures. This text was submitted by the authors in English.     

Rivers in peril inside and outside protected areas: a systematic approach to conservation assessment of river ecosystems

This paper establishes a framework within which a rapid and pragmatic assessment of river ecosystems can be undertaken at a broad, subcontinental scale, highlighting some implications for achieving conservation of river biodiversity in water‐limited countries. The status of river ecosystems associated with main rivers in South Africa was assessed based on the extent to which each ecosystem had been altered from its natural condition. This requires consistent data on river integrity for the entire country, which was only available for main rivers; tributaries were thus excluded from the analyses. The state of main river ecosystems in South Africa is dire: 84% of the ecosystems are threatened, with a disturbing 54% critically endangered, 18% endangered, and 12% vulnerable. Protection levels were measured as the proportion of conservation target achieved within protected areas, where the conservation target was set as 20% of the total length of each river ecosystem. Sixteen of the 112 main river ecosystems are moderately to well represented within protected areas; the majority of the ecosystems have very low levels of representation, or are not represented at all within protected areas. Only 50% of rivers within protected areas are intact, but this is a higher proportion compared to rivers outside (28%), providing some of the first quantitative data on the positive role protected areas can play in conserving river ecosystems. This is also the first assessment of river ecosystems in South Africa to apply a similar approach to parallel assessments of terrestrial, marine, and estuarine ecosystems, and it revealed that main river ecosystems are in a critical state, far worse than terrestrial ecosystems. Ecosystem status is likely to differ with the inclusion of tributaries, since options may well exist for conserving critically endangered ecosystems in intact tributaries, which are generally less regulated than main rivers. This study highlights the importance of healthy tributaries for achieving river conservation targets, and the need for managing main rivers as conduits across the landscape to support ecological processes that depend on connectivity. We also highlight the need for a paradigm shift in the way protected areas are designated, as well as the need for integrated river basin management plans to include explicit conservation visions, targets, and strategies to ensure the conservation of freshwater ecosystems and the services they provide.     

Akkermansia与高原牛肺水肿病相关性研究

【目的】本文通过对高原牛胃肠道菌群结构组成的分析,从微生物学角度探讨Akkermansia与高原牛肺水肿病的关系。【方法】本研究以沈阳地区健康娟姗牛为对照,以引进入拉萨半年的健康娟姗牛、拉萨本地健康黄牛以及引进入拉萨半年患肺水肿病的娟姗牛的粪便作为分析样本,采用Illumina MiSeq高通量测序技术测定样本中微生物16S rRNA基因V3–V4区序列,通过比较4种粪便样本菌群组成及丰度的差异,探讨Akkermansia与高原牛肺水肿病的相关性。【结果】Verrucomicrobia中Akkermansia在拉萨本地健康黄牛的胃肠道中的含量显著高于引进入拉萨半年的健康娟姗牛,在引进入拉萨半年患肺水肿病的娟姗牛胃肠道中的含量显著高于引进入拉萨半年的健康娟姗牛。在属水平上,沈阳地区健康娟姗牛胃肠道菌群中Akkermansia丰度占比为0.07%;引进入拉萨半年的健康娟姗牛胃肠道菌群中Akkermansia丰度占比为0.09%;拉萨本地黄牛胃肠道菌群中Akkermansia丰度占比为6.62%,是优势菌属;引进入拉萨半年的患肺水肿病的娟姗牛胃肠道菌群中Akkermansia丰度占比为11.85%,且是第一优势菌属。【结论】首次从微生物学角度探讨Akkermansia与高原牛肺水肿病的关系,为将Akkermansia丰度作为诊断肺水肿病的监测指标提供参考,但具体丰度值还有待进一步研究。     

贵州山区3种木本植物无机碳利用特性的比较

以生长在喀斯特高原地区玉舍国家森林公园内的成熟银鹊树(Tapiscia sinensis)、白栎(Quercus fabri)和亮叶桦(Betula luminifera)为实验材料,通过对光合作用、叶绿素含量、叶绿素荧光参数、羧化效率(CE)、呼吸速率(Resp)、碳酸酐酶活性(WA)以及稳定碳同位素组成(δ13 C)等指标的测定,分析3种植物不同的无机碳利用特性,为该区生态环境修复选择合适的建群植物种提供依据。结果显示:(1)银鹊树、白栎和亮叶桦分布都较为广泛,银鹊树生长的最佳土壤pH是4.5~5.5,而白栎更倾向于中性到弱酸性土壤,肥沃的酸性土壤则更有益亮叶桦生长;白栎和亮叶桦都能忍受干旱和贫瘠,但是银鹊树不能忍受干旱和高温。(2)银鹊树叶片的Pn、Tr和Gs显著大于白栎和亮叶桦,亮叶桦和白栎的Pn、Tr和Gs分别是银鹊树的69.5%、48.2%、66.7%和28.6%、21.7%、22.2%;亮叶桦叶绿素含量均为银鹊树和白栎的2倍,但3种植物间的WUE则无显著差异。(3)3个树种叶片净光合速率均随着CO2浓度升高呈持续上升的趋势,但它们之间的CO2补偿点和饱和点明显不同。其中,银鹊树和亮叶桦的CO2补偿点均低于50μmol·mol-1,而白栎的则在250~300μmol·mol-1之间;银鹊树的CO2饱和点在1 200μmol·mol-1左右,亮叶桦则在2 300μmol·mol-1左右,而白栎的CO2饱和点明显高于2 300μmol·mol-1。(4)3个树种的CE、Resp和WA均为银鹊树>亮叶桦>白栎;而δ13 C值则以银鹊树最低,亮叶桦和白栎较高。其中,白栎和亮叶桦的CE、Resp、WA分别为银鹊树的5.1%、25.7%、4.0%和45.3%、54.6%、6.8%,且树种间差异显著;白栎和亮叶桦的δ13 C值显著高于银鹊树。研究表明,银鹊树能够吸收大气中的CO2或者在高活性碳酸酐酶作用下转化利用细胞内的HCO3-,它拥有较高的CO2利用能力及无机碳同化效率,因而能够拥有较高的产能;亮叶桦只能获取大气中的CO2作为无机碳源,但它对CO2的利用能力也较高,其产能仅次于银鹊树;白栎同样只能获取大气中的CO2作为无机碳源,同时它对大气中CO2的捕获、利用能力均低于银鹊树和亮叶桦,因而白栎生长非常缓慢,造成其本身对无机碳的需求也最低,所以其产能最低。     

花椒(Zanthoxylum bungeamun)种植对喀斯特山区土壤水稳性团聚体分布及有机碳周转的影响

以贵州西南部喀斯特山区35年生和14年生花椒林为研究对象,并以未退耕旱地为对照,研究表层土壤(0~20 cm)水稳性团聚体分布及有机碳矿化特征,探讨土壤有机碳周转对不同花椒种植年限的响应。结果表明:随团聚体粒径的降低,两种年龄花椒林土壤水稳性团聚体含量呈现先增加后减少的倒"V"形分布,土壤水稳性团聚体分布主要出现在5~2、2~1和1~0.5 mm 3个粒级中;与旱地相比,花椒种植明显增加了全土和团聚体中有机碳和活性有机碳含量,并以14年生花椒林较高,而35年生花椒林存在较明显的衰减;随花椒种植年限的增加,土壤有机碳矿化累积量呈递减趋势,但土壤有机碳周转半衰期以14年生花椒林较长,显著高于旱地和35年生花椒林,表明14年生花椒林土壤有机碳更易累积,表现出较好的土壤碳固存能力;喀斯特山区种植花椒后,土壤有机碳存在"汇-源"的转换过程,因此花椒种植应注重长期维护管理,防止土壤质量的衰退。