Disturbance and climate effects on carbon stocks and fluxes across Western Oregon USA

We used a spatially nested hierarchy of field and remote‐sensing observations and a process model, Biome‐BGC, to produce a carbon budget for the forested region of Oregon, and to determine the relative influence of differences in climate and disturbance among the ecoregions on carbon stocks and fluxes. The simulations suggest that annual net uptake (net ecosystem production (NEP)) for the whole forested region (8.2 million hectares) was 13.8 Tg C (168 g C m^?2 yr^?1), with the highest mean uptake in the Coast Range ecoregion (226 g C m^?2 yr^?1), and the lowest mean NEP in the East Cascades (EC) ecoregion (88 g C m^?2 yr^?1). Carbon stocks totaled 2765 Tg C (33 700 g C m^?2), with wide variability among ecoregions in the mean stock and in the partitioning above‐ and belowground. The flux of carbon from the land to the atmosphere that is driven by wildfire was relatively low during the late 1990s (～0.1 Tg C yr^?1), however, wildfires in 2002 generated a much larger C source (～4.1 Tg C). Annual harvest removals from the study area over the period 1995–2000 were ～5.5 Tg C yr^?1. The removals were disproportionately from the Coast Range, which is heavily managed for timber production (approximately 50% of all of Oregon's forest land has been managed for timber in the past 5 years). The estimate for the annual increase in C stored in long‐lived forest products and land fills was 1.4 Tg C yr^?1. Net biome production (NBP) on the land, the net effect of NEP, harvest removals, and wildfire emissions indicates that the study area was a sink (8.2 Tg C yr^?1). NBP of the study area, which is the more heavily forested half of the state, compensated for ～52% of Oregon's fossil carbon dioxide emissions of 15.6 Tg C yr^?1 in 2000. The Biscuit Fire in 2002 reduced NBP dramatically, exacerbating net emissions that year. The regional total reflects the strong east–west gradient in potential productivity associated with the climatic gradient, and a disturbance regime that has been dominated in recent decades by commercial forestry.     

Spectral and Structural Measures of Northwest Forest Vegetation at Leaf to Landscape Scales

We report a multiscale study in the Wind River Valley in southwestern Washington, where we quantified leaf to stand scale variation in spectral reflectance for dominant species. Four remotely sensed structural measures, the normalized difference vegetation index (NDVI), cover fractions from spectral mixture analysis (SMA), equivalent water thickness (EWT), and albedo were investigated using Airborne Visible Infrared Imaging Spectrometer (AVIRIS) data. Discrimination of plant species varied with wavelength and scale, with deciduous species showing greater separability than conifers. Contrary to expectations, plant species were most distinct at the branch scale and least distinct at the stand scale. At the stand scale, broadleaf and conifer species were spectrally distinct, as were most conifer age classes. Intermediate separability occurred at the leaf scale. Reflectance decreased from leaf to stand scales except in the broadleaf species, which peaked in near-infrared reflectance at the branch scale. Important biochemical signatures became more pronounced spectrally progressing from leaf to stand scales. Recent regenerated clear-cuts (less than 10 years old) had the highest albedo and nonphotosynthetic vegetation (NPV). After 50 years, the stands showed significant decreases in albedo, NPV, and EWT and increases in shade. Albedo was lowest in old-growth forests. Peak EWT, a proxy measure for leaf area index (LAI), was observed in 11- to 30-year-old stands. When compared to LAI, EWT and NDVI showed exponentially decreasing, but distinctly different, relationships with increasing LAI. This difference is biologically important: at 95% of the maximum predicted NDVI and EWT, LAI was 5.17 and 9.08, respectively. Although these results confirm the stand structural variation expected with forest succession, remote-sensing images also provide a spatial context and establish a basis to evaluate variance within and between age classes. Landscape heterogeneity can thus be characterized over large areas—a critical and important step in scaling fluxes from stand-based towers to larger scales.     

大熊猫栖息地亚高山针叶林结构和动态特征

亚高山针叶林是大熊猫适宜的栖息环境 ,其结构和动态规律严重影响大熊猫的生存和繁衍及其进化潜力的维持 ,是恢复退化大熊猫栖息地的唯一科学依据。通过样方法和中心点四分法调查了大熊猫栖息地 4个亚高山针叶林样地和该样地所在森林的 6 2个林窗 ,研究了该类森林的结构及其更新与大熊猫主食竹生长、林窗干扰的关系 ,以期揭示亚高山针叶林的动态规律 ,为大熊猫栖息地的恢复提供科学依据。研究结果表明 :岷江冷杉 Abies faxoniana和紫果云杉 Picea purpurea是亚高山针叶林的主体 ,其所构成的森林是大熊猫重要的栖息环境。岷江冷杉种群年龄呈现连续分布格局 ,而紫果云杉种群年龄呈间歇性分布 ,其在 2 5 0～ 5 0 0 a之间没有更新。该类森林中普遍存在着林窗干扰和更新现象 ,90 %的林窗下分布有岷江冷杉和紫果云杉更新的幼苗、幼树和大树。但林窗内不同树种更新密度不同 :岷江冷杉更新幼苗、幼树和大树占所有更新树种的 82 .5 % ,而紫果云杉和糙皮桦的更新幼苗、幼树和大树占 11.3%。岷江冷杉和紫果云杉的更新同时受林下大熊猫主食竹生长状况的影响 :主食竹盖度高 ,更新树种幼苗、幼树的密度低 ,即主食竹的生长抑制了岷江冷杉和紫果云杉的更新。     

Phylogeography of Podocarpus matudae (Podocarpaceae): pre‐Quaternary relicts in northern Mesoamerican cloud forests

Aim Cloud forests of northern Mesoamerica represent the northern and southern limit of the contact zone between species otherwise characteristic of North or South America. Several phylogeographic studies featuring temperate conifer species have improved our understanding of species responses to environmental changes. In contrast, conifer species that presumably colonized northern Mesoamerica from South America are far less studied. A phylogeographic study of Podocarpus matudae (Podocarpaceae) was conducted to identify any major evolutionary divergences or disjunctions across its range and to determine if its current distribution is associated with pre‐Quaternary climatic and/or long‐distance dispersal events. Location Northern Mesoamerica (Mexico and Guatemala). Methods Sixteen populations (157 individuals) of P. matudae were screened for variation at two plastid DNA markers. The intra‐specific phylogenetic relationships among haplotypes were reconstructed using Bayesian inference. Population genetic analyses were undertaken to gain insight into the evolutionary history of these populations. To test whether genetic divergence among populations occurred at different time‐scales plastid DNA sequence data and fossil‐ and coalescent‐based calibrations were integrated. Results The combination of plastid markers yielded 11 haplotypes. Differentiation among populations based on DNA variation (G_ST) (0.707, SE 0.0807) indicated a clear population structure in P. matudae. Differentiation for ordered alleles (N_ST) (0.811, SE 0.0732) was higher than that for G_ST, indicating phylogeographical structure in P. matudae. Most of the total variation (81.3%, P < 0.0001) was explained by differences among populations. The estimated divergence time between the unique haplotypes from a Guatemalan population and the two most common haplotypes from the Sierra Madre Oriental in Mexico was between 10 and 20 Ma, and further haplotype divergence in the poorly resolved clade of the Sierra Madre Oriental occurred between 3 and 0.5 Ma. Main conclusions Divergence estimations support the hypothesis that extant Podocarpus matudae populations are pre‐Quaternary relicts. This finding is consistent with fossil and pollen data that support a Miocene age for temperate floristic elements in Mesoamerican cloud forests, whereas further haplotype divergence within the Sierra Madre Oriental, Chiapas and Guatemala occurred more recently, coinciding with Pleistocene cloud forest refugia.     

凉水自然保护区松鼠的越冬行为策略

在2006 年冬季预观察的基础上,于2007 年10 月31 日至2008 年3 月25 日在40 hm2 范围内使用无线电颈圈和彩色塑料颈圈标记8 只松鼠。结合无线电追踪技术和雪地痕迹技术,采用目标取样法对凉水自然保护区冬季松鼠行为进行了连续21 周的定位观察,以研究松鼠行为节律、空间行为和重取行为对冬季低温条件的响应。结果表明,松鼠冬季的活动节律为单峰型,随着气温的下降显著延后出巢时间(Kendall τ test;n = 21,r =- 0.92,τ = - 0.86,P < 0. 0001), 缩短活动时长(Kendall τ test; n = 21,r =0.80,τ = 0.68,P <0.0001)。松鼠冬季家域近似椭圆形(面积2.46 ±0.09 hm² ), 未见个体间家域重叠。秋季松鼠将红松种子分散贮藏于整个家域范围内,但重取行为相对集中于几个主要区域(重取区)。依据巢和重取区的位置特征及其利用率可将家域划分为3 个部分:主区位于家域的中段,辅区靠近红松母树林,次辅区位于家域远离红松母树林一侧。贮藏的红松种子是松鼠冬季唯一的食物来源。在冬季的不同阶段,松鼠对不同重取区的利用率显著不同(初冬,Kruskal-
Wallis test;df = 2, x² = 5.65, P = 0.0594; 隆冬,Kruskal-Wallis test;df = 2,x² = 14.24, P = 0.0008; 晚冬,One-Way ANOVA Test,df = 2,18, F = 7.00,P = 0.0056), 位于主区(初冬利用率37.8 ± 7.7% ,隆冬利用率80.5 ±9.2% ,晚冬利用率40.5 ±2.7% )和辅区(初冬利用率41.8 ± 5.9% ,隆冬利用率14.8 ± 9.2% ,晚冬利用率37.8 ± 4.9% )的重取区是松鼠的主要重取区。随着时间推移空取率显著提高(Kruskal-Wallis test;df = 2,x² = 16.60,P = 0.0002)的现象提示松鼠很可能依靠空间记忆取回贮藏的食物。轮换利用多个巢(6 ± 1)有助于降低松鼠被天敌捕食的风险。这些巢都分布在重取区附近,巢的利用与重取区的利用显著相关(Kendall τ test;主区:n = 217,r = 0.79,τ = 0.6256,P = 0.0003;辅区:n = 171,r = 0.67,τ = 0.6186,P = 0.0006;次辅区:n = 88,r = 0.74,τ = 0.6565,P = 0.0006),松鼠通常取食后即直接进入就近的巢过夜,有助于松鼠减少
能量损耗。多域集中重取及相应的巢轮换策略是松鼠对冬季低温环境及天敌捕食压力的综合响应。     

落叶阔叶林冠层光合有效辐射分量的遥感模拟与分析

冠层绿色叶片(光合组分)的光合有效辐射分量(绿色FPAR)真实地反映了植被与外界进行物质和能量交换的能力,获取冠层光合组分吸收的太阳光合有效辐射,对生态系统生产力的遥感估算精度的提高具有重要的意义。研究以落叶阔叶林为例,基于SAIL模型模拟森林冠层光合组分和非光合组分吸收的光合有效辐射,研究冠层FPAR变化规律以及与植被指数的相关关系。结果表明,冠层结构的改变会影响冠层对PAR的吸收能力,冠层绿色FPAR的大小与植被面积指数及光合组分面积比相关;在高覆盖度植被区,冠层绿色FPAR占冠层总FPAR的80%以上,非光合组分的贡献较小,但在低植被覆盖区,当光合组分和非光合组分面积相同时,绿色FPAR不及冠层总FPAR的50%;相比于NDVI,北方落叶阔叶林冠层EVI与绿色FPAR存在更为显著的线性相关关系(R~20.99)。     

Multiple introductions,admixture and bridgehead invasion characterize the introduction history of Ambrosia artemisiifolia in Europe and Australia

Admixture between differentiated populations is considered to be a powerful mechanism stimulating the invasive success of some introduced species. It is generally facilitated through multiple introductions; however, the importance of admixture prior to introduction has rarely been considered. We assess the likelihood that the invasive Ambrosia artemisiifolia populations of Europe and Australia developed through multiple introductions or were sourced from a historical admixture zone within native North America. To do this, we combine large genomic and sampling data sets analysed with approximate Bayesian computation and random forest scenario evaluation to compare single and multiple invasion scenarios with pre‐ and postintroduction admixture simultaneously. We show the historical admixture zone within native North America originated before global invasion of this weed and could act as a potential source of introduced populations. We provide evidence supporting the hypothesis that the invasive populations established through multiple introductions from the native range into Europe and subsequent bridgehead invasion into Australia. We discuss the evolutionary mechanisms that could promote invasiveness and evolutionary potential of alien species from bridgehead invasions and admixed source populations.     

A phylogeographic investigation of the kelp genus Laminaria (Laminariales,Phaeophyceae), with emphasis on the South Atlantic Ocean

The genus Laminaria has a wide distribution range compared with other kelp genera because it is found in both the North and the South Atlantic, on both sides of the North Pacific, as well as in the Mediterranean. Hypotheses behind this biogeographical pattern have been discussed by several authors but have not yet been fully evaluated with time‐calibrated phylogenies. Based on the analysis of four molecular markers (ITS2, rbcL, atp8 and trnWI), our goal was to reassess the Laminaria species diversity in South Africa, assess its relationship with the other species distributed in the South Atlantic and reconstruct the historical biogeography of the genus. Our results confirm the occurrence of a single species, L. pallida, in southern Africa, and its sister relationship with the North Atlantic L. ochroleuca. Both species belonged to a clade containing the other South Atlantic species: L. abyssalis from Brazil, and the Mediterranean L. rodriguezii. Our time‐calibrated phylogenies suggest that Laminaria originated in the northern Pacific around 25 mya, followed by at least two migration events through the Bering Strait after its opening (~5.32 mya). Today, the first is represented by L. solidungula in the Arctic, while the second gave rise to the rest of the Atlantic species. The colonization of the North Atlantic was followed by a gradual colonization southward along the west coast of Europe, into the Mediterranean (~2.07 mya) and two recent, but disconnected, migrations (~1.34 and 0.87 mya) across the equator, giving rise to L. abyssalis in Brazil and L. pallida in southern Africa, respectively.