山西霍山灌丛空隙草本植物物种多样性与更新

采用物种重要值和物种多样性指数,分析了山西霍山灌丛空隙内主要草本组成及其多样性随灌丛空隙面积梯度的变化规律。结果表明:在自然状况下形成的10 m2的灌丛空隙最多,占51.2%。灌丛空隙内草本植物的重要值高于灌丛下草本,且以10~20 m2的空隙为最高。主要草本可分为3类:(1)对灌丛空隙更新反应不明显的草本,(2)对灌丛空隙有正更新反应的草本,(3)对灌丛空隙有负更新反应的草本。灌丛空隙内的物种丰富度、多样性指数和均匀度指数均高于灌丛下,而生态优势度均小于灌丛下,呈现"单峰型"的变化趋势,且在10~20 m2达到峰值。因此,适宜大小的灌丛空隙是森林生态系统草本层植物多样性维持的重要途径。     

Reconstruction of disturbance history of a typical broad-leaved Pinus koraiensis forest and mechanisms of disturbance occurrence

该文依托于小兴安岭典型阔叶红松(Pinus koraiensis)林9 hm2森林动态监测样地,对样地内林窗边缘主要树种红松和臭冷杉(Abies nephrolepis)进行生长释放判定分析,重建了冠层树木的干扰历史。结果表明:整体上林窗木与非林窗木的生长变化百分率变化规律基本一致,而不同林窗间生长变化百分率存在明显的差异,林窗干扰及其产生的影响存在较大的变异性。在1733–1738、1748–1752、1769–1771、1798–1801、1827–1833、1841–1844、1935–1939及1968–1973年间红松生长释放较强,其中1752、1770、1800、1830、1842、1937及1970年出现了明显的干扰峰;在1889–1904、1932–1938、1947–1973和1986–2005年间臭冷杉生长释放较强,其中1894、1934、1951、1968和1990年出现了明显的干扰峰。红松干扰存在2.0 a、3.5 a、3.8 a、7.3–7.9 a和9.1–18.2 a的显著周期,臭冷杉干扰存在3.5–3.6 a、7.5–48.8 a和65–85 a的显著周期。风干扰是典型阔叶红松林干扰释放的主要因子,异常温度也影响该地区树木生长释放事件。太阳活动通过影响局地风速、温度、降水等气候因子以及其他大尺度气候模态影响林窗动态,可能是小兴安岭典型阔叶红松林的干扰机制之一。     

Études stratigraphique,sédimentologique et paléomagnétique des travertins de Kocabaş, Bassin de Denizli,Anatolie, Turquie,contenant des restes fossiles quaternaires

Stratigraphic, sedimentological and paleomagnetic studies were conducted on the travertine from Denizli Basin, near Kocabas village, in the Denizli region in Turkey, following the paleontological discovery in 2002. The stratigraphic and sedimentological studies show at least two main cycles of mass travertine, separated by a fluvial deposit and overlain by a fluvio-lacustrine deposit. These travertines must have formed in environments with strong hydrodynamics (streams or waterfalls) and are preferentially located at breaks of slopes. The paleomagnetic study shows that all the quarry travertine presents reverse magnetic polarity. On the other hand, the detrital fluvio-lacustrine deposit above the travertine presents normal geomagnetic polarity, except at the top, where it is reversed. Given the presence of an archaic Homo erectus skull and Villafranchian paleontological remains in the upper travertine unit, the whole travertine dates from the upper Matuyama, and is more recent than the Olduvai event (1.78 Ma). The normal polarity recorded in the upper fluvio-lacustrine deposit could correspond to the Cobb Mountain excursion, dated to 1.22 Ma.     

The coconut palm,Cocos nucifera,impacts forest composition and soil characteristics at Palmyra Atoll,Central Pacific

Question: Cocos nucifera, the coconut palm, has a pantropical distribution and reaches near monodominance in many atolls, low lying islands and coastal regions. This paper examines the ecological correlation between C. nucifera abundance and changes in forest structure, floristic diversity and forest soil characteristics. Location: Palmyra Atoll NWR (USA), Central Pacific Ocean. Methods: Plant surveys were conducted on 83 transects (each 100 m²). All plants ≥5 cm in height were identified and counted; large plants were also measured and ground cover was surveyed. Major macronutrients, pH, macro‐elements/base cations, micronutrients and pedogenic elements, and thermodynamic stability levels were quantified from soil samples taken at each transect. Results: Even in a low diversity atoll environment, we found that high abundances of C. nucifera corresponded with pronounced differences in forest communities including: lower diversity of established trees and regenerating understorey; higher stem density and stand basal area; lower abundance of major macronutrients; and differences in macro and trace elements and energy content of soil organic matter. Historical natural experiments document that the expansion of C. nucifera was the likely causative agent of these changes. Discussion: Cumulatively, these data show that C. nucifera has important impacts on floristic, structural and soil characteristics of forests where it becomes dominant. Given the high proportion of tropical coastal areas in which C. nucifera is now naturalized and abundant, this likely has important implications for coastal forest diversity and structure.     

秦岭植物区系一新记录科——茶茱萸科

首次报道了茶茱萸科(Icacinaceae)假柴龙树属(Nothapodytes Bl.)马比木[Nothapodytes pittosporoides (Oliv.) Sleum.]在秦岭南坡(陕西省山阳县)的分布,为秦岭植物区系增加一新记录科--茶茱萸科     

金秀大瑶山瑶民“鸟盆”狩猎区鸟类食物源植物及生态保育

2003年7月～2008年12月,对金秀大瑶山茶山瑶民"鸟盆"狩猎活动区域的鸟类食物源植物进行了调查,录得"鸟盆"狩猎区秋冬季鸟类取食果实、种子的植物有28科71种,当地称为"鸟果"树。此外,瑶民"鸟盆"狩猎活动所需的"鸟漆"(粘捕鸟类的粘胶)是用9种冬青科植物的树皮制作,其果实、种子亦是"鸟盆"狩猎活动区鸟类的主要食物。     

广东省南昆山伯乐树群落特征及其保护策略

在广东省南昆山自然保护区内调查了中国特有珍稀植物伯乐树种群的分布格局、龄级结构和伴生群落的物种组成.结果表明:该种群的分布范围狭窄且集中;龄级不完整,Ⅱ、Ⅲ级幼树少见,结构呈衰退型;伴生群落呈典型的亚热带植物区系的特点,其组成不稳定、优势种不显著.建议将伯乐树幼树作为就地保护的重点,适当去除周围的罗浮槭、羊角杜鹃和黄樟等速生树种,以创造有光照和水肥条件的生境;对于Ⅳ级以上成株,应注意拟赤杨和华润楠等空间生态位相近树种的数量和密度,适当疏剪枝条,以帮助成株占据较好的空间位;同时再积极引入异龄的伯乐树幼苗,促进种群恢复和发展.     

2000～2008年长白山地区植被覆盖变化特征

利用2000～2008年250 m分辨率MODIS/NDVI数据,结合谐波分析、影像处理和多种统计方法分析长白山地区的植被覆盖年内和年际变化特征,并结合区划图和植被类型图对不同区域和不同植被类型的植被覆盖变化进行分析.结果显示:近9年长白山地区覆盖总体呈上升趋势,其中春季植被覆盖略有下降,夏季植被覆盖变化不大,而秋季植被覆盖显著上升;和龙林业局、露水河林业局和长白山自然保护区的植被覆盖较好,而朝鲜一侧、泉阳林业局和长白林业局的植被覆盖较差;针叶林、阔叶林和针阔混交林的植被覆盖要高于荒草地、沼泽地、高山岳桦林和高山苔原,但后几种植被类型的植被覆盖增长趋势明显.     

淀山湖基于初级生产力的鲢鳙富营养化控制

于2008年10月—2009年9月,采用黑白瓶测溶氧法对淀山湖湖南区和围隔区初级生产力进行逐月测定,依据测定的湖南区初级生产力估算鲢、鳙渔产潜力及合理放养量,讨论温度、透明度、营养盐、叶绿素a等理化因子与初级生产力的相关性,分析鲢、鳙放养对淀山湖水体营养物质的定量去除效果。结果表明:1)湖南区平均水柱日毛产量(PG)为4.02gO2.m-2,8月最高、1月最低,净产量(PN)为1.99gO2.m-2,年PN/PG=52%;2)0～0.5m水层对水柱初级生产力贡献最大,湖南区占32.3%、围隔区占32.2%;3)初级生产力与透明度、水温呈明显正相关,与其他理化因子相关性不明显;4)淀山湖浮游植物年生产量为28.18×104t,按鲢鳙3:1比例放养,鲢渔产潜力为1621.58t,鳙为1216.18t,鲢合理放养量为16.94t.km-2,鳙合理放养量为6.35t.km-2;5)以淀山湖每年渔产2837.76t计算,可以固定氮、磷分别为85.50t、7.63t,由此可使淀山湖水体中氮、磷含量分别降低0.67和0.06mg.L-1。     

Leaf gas exchange and water status responses of a native and non-native grass to precipitation across contrasting soil surfaces in the Sonoran Desert

Arid and semi-arid ecosystems of the southwestern US are undergoing changes in vegetation composition and are predicted to experience shifts in climate. To understand implications of these current and predicted changes, we conducted a precipitation manipulation experiment on the Santa Rita Experimental Range in southeastern Arizona. The objectives of our study were to determine how soil surface and seasonal timing of rainfall events mediate the dynamics of leaf-level photosynthesis and plant water status of a native and non-native grass species in response to precipitation pulse events. We followed a simulated precipitation event (pulse) that occurred prior to the onset of the North American monsoon (in June) and at the peak of the monsoon (in August) for 2002 and 2003. We measured responses of pre-dawn water potential, photosynthetic rate, and stomatal conductance of native (Heteropogon contortus) and non-native (Eragrostis lehmanniana) C₄ bunchgrasses on sandy and clay-rich soil surfaces. Soil surface did not always amplify differences in plant response to a pulse event. A June pulse event lead to an increase in plant water status and photosynthesis. Whereas the August pulse did not lead to an increase in plant water status and photosynthesis, due to favorable soil moisture conditions facilitating high plant performance during this period. E. lehmanniana did not demonstrate heightened photosynthetic performance over the native species in response to pulses across both soil surfaces. Overall accumulated leaf-level CO₂ response to a pulse event was dependent on antecedent soil moisture during the August pulse event, but not during the June pulse event. This work highlights the need to understand how desert species respond to pulse events across contrasting soil surfaces in water-limited systems that are predicted to experience changes in climate.