Evaluation of phosphorus distribution and bioavailability in sediments of a subtropical wetland reserve in southeast China

The phosphorus (P) fractions and bioavailable P in the sediments from the Quanzhou Bay Estuarine Wetland Nature Reserve were investigated using chemical extraction methods for the first time to study the distribution and bioavailability of P in the reserve sediments. A hypothesis was presented suggesting that the bioavailable P in the sediments could be evaluated using the P fractions. The total phosphorus (TP), inorganic phosphorus (IP), organic phosphorus (OP), non-apatite phosphorus (NAIP), and apatite phosphorus (AP) contents in the sediments were in the ranges of 303.87–761.59 mg kg⁻¹, 201.22–577.66 mg kg⁻¹, 75.83–179.16 mg kg⁻¹, 28.86–277.90 mg kg⁻¹, and 127.36–289.94 mg kg⁻¹, respectively. The water soluble phosphorus (WSP), readily desorbable phosphorus (RDP), algal available phosphorus (AAP), and NaHCO₃ extractable phosphorus (Olsen-P) contents in the sediments were in the ranges of 0.58–357.17 mg kg⁻¹, 80.77–586.75 mg kg⁻¹, 1.09–24.12 mg kg⁻¹, and 54.96–676.82 mg kg⁻¹, respectively. The correlation analysis results showed that the NAIP was the major component of the bioavailable P and that the impact of the AP on the bioavailable phosphorus may be minimal. Due to the low TP content in the sediments of the Quanzhou Bay Estuarine Wetland Nature Reserve, the potential pollution risks of P in the sediments may not be very high. The results also show that the bioavailable P concentrations in the sediments of the Quanzhou Bay Estuarine Wetland Nature Reserve could not be evaluated by measuring the P fractions and that the hypothesis was untenable.     

Phylogeography and climatic niche evolution in live oaks (Quercus series Virentes) from the tropics to the temperate zone

Aim We investigated the phylogeography, geographical variation in leaf morphology, freezing tolerance and climatic niches of two widespread evergreen sister oak species (Quercus) in the series Virentes. Location South‐eastern USA, Mexico and Central America. Methods Nuclear microsatellites and non‐recombining nuclear and chloroplast DNA sequences were obtained from trees throughout the range of two sister lineages of live oaks, represented by Quercus virginiana in the temperate zone and Q. oleoides in the tropics. Divergence times were estimated for the two major geographical and genetic breaks. Differentiation in leaf morphology, analysed from field specimens, was compared with the molecular data. Freezing sensitivities of Q. virginiana and Q. oleoides populations were assessed in common garden experiments. Results The geographical break between Q. virginiana and Q. oleoides was associated with strong genetic differentiation of possible early Pleistocene origin and with differentiation in freezing sensitivity, climatic envelopes and leaf morphology. A second important geographical and genetic break within Q. oleoides between Costa Rica and the rest of Central America showed a mid‐Pleistocene divergence time and no differentiation in leaf morphology. Population genetic differentiation was greater but genetic diversity was lower within the temperate Q. virginiana than within the tropical Q. oleoides, and genetic breaks largely corresponded to breaks in leaf morphology. Main conclusions Two major breaks, one between Mexico and the USA at the boundary of the two species, and a more recent one within Q. oleoides between Honduras and Costa Rica, implicate climatic changes as potential causes. The latter break may be associated with the formation of the Cordillera de Guanacaste, which was followed by seasonal changes in precipitation. In the former case, an ‘out of the tropics’ scenario is hypothesized, in which the acquisition of freezing tolerance in Q. virginiana permitted colonization of and expansion in the temperate zone, while differences in climatic tolerances between the species limited secondary contact. More pronounced Pleistocene changes in climate and sea level in the south‐eastern USA relative to coastal Mexico and Central America may explain the greater population differentiation within temperate Q. virginiana and greater genetic diversity in tropical Q. oleoides. These patterns are predicted to hold for other taxa that span temperate and tropical zones of North and Central America.     

Leaf damage by herbivore feeding guilds along gradients of elevation and plant species richness

The proportion of leaves damaged by specialist guilds such as miners and sap-feeders decreased at locations with higher species richness and at higher elevation in four subtropical forest seedling communities in south China. The effect of elevation was stronger in winter. Patterns of the generalist guild chewers were weaker.     

广西天然林中藤本植物区系组成及系统发育多样性

藤本植物是热带和亚热带森林的重要组分,在过去几十年中藤本植物多样性在热带森林增加,有可能导致森林的多样性减少,碳储量等生态系统服务功能降低,引起广泛关注。以《广西植被志要》中共355个样地数据(喀斯特森林、海拔1000 m以下的非喀斯特森林和海拔1000 m以上的非喀斯特森林)为基础,结合气候数据,分析天然林中藤本植物区系组成、不同生境藤本植物物种多样性与系统发育多样性关系、藤本植物物种多样性与年平均温度关系,以及系统发育结构特点。结果表明:(1)广西天然林藤本植物中,热带分布的含藤属占比最大(75.4%),温带分布含藤属占比较低(12.3%),世界广布含藤属和亚洲分布含藤属占比最小,海拔1000 m以下的喀斯特和非喀斯特森林都有一些专有的含藤科属;(2) 3个生境藤本的Gleason物种多样性和系统发育多样性与年均温都不相关,它们的物种多样性差异不显著,但是系统发育多样性有显著差异,海拔1000 m以下的非喀斯特森林中系统发育多样性最高,喀斯特森林系统发育多样性最低;(3)非喀斯特森林藤本植物系统发育结构趋向于离散,暗指竞争排斥作用是藤本植物组合在该生境群落主要构建机制,喀斯特森林藤本植物系统发育结构趋向于聚集,暗指藤本植物组合由生境过滤作用为主形成。这些研究发现对于热带亚热带森林藤本植物的多样性组成及其共存机制提供了新认识。     

氮磷添加对杉木林土壤碳氮矿化速率及酶动力学特征的影响

以江西杉木林红壤为研究对象,开展野外长期氮(N)、磷(P)添加控制试验,设置对照(CK)、N(50kg N hm~(-2)a~(-1))、P(50kg P hm~(-2)a~(-1))、NP(50kg N hm~(-2)a~(-1)+50kg P hm~(-2)a~(-1))处理,分析N、P添加对土壤碳矿化速率(C_(min))、氮矿化速率(N_(min))和相关的β-1,4-葡萄糖苷酶(βG)和β-1,4-N-乙酰葡糖氨糖苷酶(NAG)动力学参数的影响。结果表明:(1)N添加明显降低了C_(min)和N_(min),比CK分别减少了25%和18%;N添加减小了NAG的潜在最大酶活性(V_(max))、半饱和常数(K_m)、催化效率(V_(max)/K_m),但差异不显著(P0.05);N添加显著增加了βG的V_(max)、K_m,但对V_(max)/K_m有抑制作用。(2)P输入(P、NP)较CK使NAG的V_(max)、K_m减小26%—60%;NP同时添加明显提高βG和NAG的V_(max)/K_m(P0.05),但P输入(P、NP)对C_(min)和N_(min)影响不显著(P0.05)。(3)C_(min)与土壤溶解性有机碳正相关,N_(min)与pH显著正相关,与土壤NH_4~+-N、NO_3~--N显著负相关;βG和NAG的V_(max)/K_m均与NH_4~+-N、NO_3~--N负相关(P0.05),K_m均与NH_4~+-N、NO_3~--N正相关(P0.05)。βG的V_(max)与NH_4~+-N、NO_3~--N正相关(P0.05),NAG的V_(max)与有机碳、全氮、全磷、有效磷负相关(P0.05)。研究结果表明,在亚热带杉木人工林中,N添加降低土壤pH,增加土壤有效氮含量,抑制βG和NAG的V_(max)/K_m,对土壤C_(min)和N_(min)产生抑制作用;而NP添加增加土壤有效磷含量,增加土壤βG和NAG的V_(max)/K_m。     

模拟增温对中亚热带杉木人工林土壤磷有效性的影响

气候变暖改变与土壤磷循环相关的生物地球化学过程,对陆地生态系统磷循环产生直接或间接影响。为研究亚热带地区杉木人工林土壤磷有效性对增温的响应,开展了模拟增温实验。实验设置对照组及增温组(5℃),经过1.5a的短期增温,对杉木人工林的土壤全磷、有机磷、微生物量磷、有效磷、酸性磷酸酶活性及相关土壤理化性质进行测定,结果表明:增温处理下,土壤酸性磷酸酶活性提高约1.5倍,土壤全磷、微生物量磷以及有机磷含量分别减少了6%、34%和12%,土壤有效磷含量增加25%。可见,短期增温通过提高土壤磷酸酶活性进而促进土壤有机磷矿化和降低土壤微生物固磷量,从而增加土壤磷有效性,但是增温导致潜在可利用的土壤微生物量磷大幅度的降低,将有可能加剧亚热带杉木人工林土壤磷限制。     

Native woody vegetation in central Argentina: Classification of Chaco and Espinal forests

Question

What are the composition and spatial patterns of native woody plant communities in the southern Great Chaco and Espinal?

Location

Córdoba Province, central Argentina, an area of ca. 161,000 km².

Methods

We collected 351 geo‐referenced relevés representative of the geographic, topographic and ecological variation of the Chaco and Espinal woody vegetation in central Argentina. The relevés were classified into vegetation types using the hierarchical ISOPAM method. Forest and shrubland types were described on the basis of diagnostic species occurrences and their distribution in relation to environmental factors. A map of the actual vegetation derived from remote‐sensed images (Landsat) and field data was used to describe the current distribution and abundance of the different vegetation types.

Results

The classification of the 351 plots × 837 species matrix revealed two major clusters comprising seven woody vegetation types corresponding to Chaco lowland and mountain forests and shrublands, Espinal forests and edaphic vegetation. The most important gradients in woody vegetation types are related to elevation, temperature and rainfall variables.

Conclusions

Subtropical seasonally dry woody plant communities from the southern extreme of the Great Chaco and Espinal forests were described for the first time based on complete floristic data. Our results show that lowland Chaco native forests, as well as replacement communities, are still present in its southern distribution range and are well distinguishable from other vegetation types such as the Espinal and mountain forests. Overall, extensive Espinal forests have almost disappeared while Chaco vegetation is highly fragmented and degraded.

     

山东南部景观生态对策研究

在对山东南部气候、地貌、土壤、植被等景观生态要素研究的基础上,以地貌和基质为基本线索、以植被为标志建立了该地区的景观生态分类系统．该系统为二级分类系统,包括７个景观型、１７个景观亚型,其中,景观型根据植被（植被型或栽培植被型）划分,景观亚型根据地貌、植被（群系组或栽培组合）划分．以景观亚型或景观亚型的组合为基本单位,以１∶１００万土壤图为基础底图,参考多种比例尺的卫星照片、植被图、土地利用图、地貌图等,编制了山东南部１∶１００万景观生态类型图;在景观生态类型图上量算了各景观亚型的面积．据此详细分析了山东南部稀疏植被景观、常绿针叶林景观、落叶阔叶林景观、旱地作物景观、水旱轮作景观、湖泊景观等主要景观型的生态问题,提出了相应的生态对策     

广东黑石顶南亚热带常绿阔叶林树木生长研究(英文)

用测树器和年轮解析法 ,测定了广东黑石顶南亚热带常绿阔叶林的立木和幼树的径向生长和高生长。年轮解析法测得立木的年直径生长量在 0 .1～ 0 .5cm之间 ,一些立木的直径生长呈现出生长快的年份 ( 1～ 3a)和生长慢的年份 ( 1～ 3a)交替的节律。测树器测得立木 5a的年平均直径生长量为0 .0 74cm,5年期间测得有 1 7.6%的个体直径为零增长或负增长。立木的年高增长量为 1 0～ 50 cm,高生长高峰期通常在 1 0～ 30年龄。在树木生长的早期 ,高度的生长优于直径的生长 ,而在树木生长的中、后期 ,直径的生长逐渐优于高度的生长。用游标卡尺和卷尺测得幼树 (通常 1～ 3m高 )的直径和高度 5a的平均生长量分别为 0 .1 0 7cm和 4.76cm。 5a间没有幼树的直径生长为零增长或负增长 ,但约有 9%的个体的高度生长为零增长或负增长。