PHYSIOLOGICAL RESPONSES OF ECKLONIA RADIATA (LAMINARIALES) TO A LATITUDINAL GRADIENT IN OCEAN TEMPERATURE1

We tested the ability of sporophytes of a small kelp, Ecklonia radiata (C. Agardh) J. Agardh, to adjust their photosynthesis, respiration, and cellular processes to increasingly warm ocean climates along a latitudinal gradient in ocean temperature (～4°C). Tissue concentrations of pigment and nutrients decreased with increasing ocean temperature. Concurrently, a number of gradual changes in the metabolic balance of E. radiata took place along the latitudinal gradient. Warm‐acclimatized kelps had 50% lower photosynthetic rates and 90% lower respiration rates at the optimum temperature than did cool‐acclimatized kelps. A reduction in temperature sensitivity was also observed as a reduction in Q₁₀‐values from cool‐ to warm‐acclimatized kelps for gross photosynthesis (Q₁₀: 3.35 to 1.45) and respiration (Q₁₀: 3.82 to 1.65). Respiration rates were more sensitive to increasing experimental temperatures (10% higher Q₁₀‐values) than photosynthesis and had a higher optimum temperature, irrespective of sampling location. To maintain a positive carbon balance, E. radiata increased the critical light demand (E_c) exponentially with increasing experimental temperature. The temperature dependency of E_c was, however, weakened with increasing ocean temperature, such that the critical light demand was relaxed in kelp acclimated to higher ocean temperatures. Nevertheless, calculations of critical depth limits suggested that direct effects of future temperature increases are unlikely to be as strong as effects of reduced water clarity, another globally increasing problem in coastal areas.     

Soil water availability and rooting depth as determinants of hydraulic architecture of Patagonian woody species

Adaptations of species to capture limiting resources is central for understanding structure and function of ecosystems. We studied the water economy of nine woody species differing in rooting depth in a Patagonian shrub steppe from southern Argentina to understand how soil water availability and rooting depth determine their hydraulic architecture. Soil water content and potentials, leaf water potentials (Ψ_Leaf), hydraulic conductivity, wood density (ρ_w), rooting depth, and specific leaf area (SLA) were measured during two summers. Water potentials in the upper soil layers during a summer drought ranged from −2.3 to −3.6 MPa, increasing to −0.05 MPa below 150 cm. Predawn Ψ_Leaf was used as a surrogate of weighted mean soil water potential because no statistical differences in Ψ_Leaf were observed between exposed and covered leaves. Species-specific differences in predawn Ψ_Leaf were consistent with rooting depths. Predawn Ψ_Leaf ranged from −4.0 MPa for shallow rooted shrubs to −1.0 MPa for deep-rooted shrubs, suggesting that the roots of the latter have access to abundant moisture, whereas shallow-rooted shrubs are adapted to use water deposited mainly by small rainfall events. Wood density was a good predictor of hydraulic conductivity and SLA. Overall, we found that shallow rooted species had efficient water transport in terms of high specific and leaf specific hydraulic conductivity, low ρ_w, high SLA and a low minimum Ψ_Leaf that exhibited strong seasonal changes, whereas deeply rooted shrubs maintained similar minimum Ψ_Leaf throughout the year, had stems with high ρ_w and low hydraulic conductivity and leaves with low SLA. These two hydraulic syndromes were the extremes of a continuum with several species occupying different portions of a gradient in hydraulic characteristics. It appears that the marginal cost of having an extensive root system (e.g., high ρ_w and root hydraulic resistance) contributes to low growth rates of the deeply rooted species.     

Spacer elongation and plagiotropic growth are the primary clonal strategies used by Vallisneria spiralis to acclimate to sedimentation

The aim of this study is to identify how submerged macrophyte Vallisneria spiralis acclimate to sedimentation by investigating the growth, biomass allocation and clonal characteristics in a greenhouse experiment of 30 days. Experimental treatments combined two sediment types (mud and sand) with four sedimentation depths (0, 2, 4 and 8 cm) in a factorial design. Biomass accumulation (0.98–1.33 versus 0.36 g per plant) and relative growth rate (RGR, 0.082–0.093 versus 0.046 g g⁻¹ day⁻¹) decreased only in the 8 cm sand treatment. Neither sedimentation depth nor sediment type influenced biomass allocation. The ratio of spacer length to biomass was significantly higher in the 8 cm sand (20.4 cm g⁻¹) than in other treatments (6.0–8.5 cm g⁻¹). Branching angles and the depths between ramet basal and sediment surface were only affected by sedimentation depth. Clonal ramets developed nearly vertical branching angles (ranged from 78° to 101°) in the 0 cm sedimentation treatment, but the angles of treated plants decreased at the initial 3–5 ramets (ranged from 68° to 78° at the first ramet level), then remained a relatively constant value (about 90°) in the following spacers. These data indicate that plagiotropic stolons were formed to project the ramets to sediment surface and to escape sedimentation stress primarily by elongating spacer length and decreasing branching angle, rather than by adjusting biomass allocation.     

Foraging behavior of Adélie penguins during incubation period in Lützow-Holm Bay

The diving behavior of Adélie penguins Pygoscelis adeliae was investigated using time–depth recorders during the incubation period in the fast sea-ice area of Lützow-Holm Bay, Antarctica. Dive profiles and activity/time allocation suggested that penguins were obligated to walk on the fast-ice for 90–100 km until a polynya, which they used as an access to the pack-ice zone. Dive depth did not differ between males and females, though males’ dive duration was longer than that of females. Dive depth was slightly shallower and dive duration was shorter during the incubation than during the chick-rearing phase. Birds dove throughout the day, although less frequently around midnight, and there was no clear diel change in dive depth. This daily dive pattern during incubation period was similar to that previously observed during the chick-rearing period in a fast sea-ice area, but differed from that observed in sea-ice-free area. Variations in diving behavior resulted from different environmental conditions, such as foraging area with different sea-ice condition, as well as from different life history strategies.     

Rapoport's bathymetric rule and the latitudinal species diversity gradient for Northeast Pacific fishes and Northwest Atlantic gastropods: evidence against a causal link

Aim Few studies have explicitly considered the recurrent pattern of declining species diversity and increasing geographical range size that exists for numerous taxa across a variety of physical gradients. We extend Stevens’ [ Stevens, G.C. (1996) Journal of Biogeography, 23 , 149] work on Rapoport's bathymetric rule, using a more complete latitudinal assemblage of Northeast Pacific fishes and new data from Northwest Atlantic gastropods, to show that bathymetrical range size and species diversity are not causally linked. Location Fishes from the Northeast Pacific (0°–60° N) and gastropods from the Northwest Atlantic (0°–74° N) distributed from the surface to depths greater than 200 m. Methods Species pools were divided into three bathymetrical subgroups: (1) species restricted to shallow waters, between the surface and 200 m, (2) species that occurred in waters, both shallow and deep of 200 m, and (3) species restricted to waters deeper than 200 m. Median bathymetrical range size and total number of species were plotted against latitude (2° bins) using Stevens’ method, for the entire species pool and individual bathymetrical groups. Results For both fishes and gastropods, the apparent link between extratropical diversity and bathymetrical range size is an artefact resulting from the disproportionately high number of shallow restricted species in tropical latitudes, and the loss of these species in temperate latitudes. Furthermore, the extratropical gradient in gastropod diversity and bathymetrical range size are decoupled by approximately 15°, and while the latitudinal pattern for diversity is consistent across bathymetrical groups, median bathymetrical range size is highly irregular. Main conclusions These results suggests that functional groups can contribute disproportionately to patterns apparent at larger scales and that analysis of ecographical patterns by subregion is a novel approach that can help resolve debates over causality when patterns are seemingly coincident.     

Experimental evidence for the attenuating effect of SOM protection on temperature sensitivity of SOM decomposition

The ability to predict C cycle responses to temperature changes depends on the accurate representation of temperature sensitivity (Q₁₀) of soil organic matter (SOM) decomposition in C models for different C pools and soil depths. Theoretically, Q₁₀ of SOM decomposition is determined by SOM quality and availability (referred to here as SOM protection). Here, we focus on the role of SOM protection in attenuating the intrinsic, SOM quality dependent Q₁₀. To assess the separate effects of SOM quality and protection, we incubated topsoil and subsoil samples characterized by differences in SOM protection under optimum moisture conditions at 25 °C and 35 °C. Although lower SOM quality in the subsoil should lead to a higher Q₁₀ according to kinetic theory, we observed a much lower overall temperature response in subsoil compared with the topsoil. Q₁₀ values determined for respired SOM fractions of decreasing lability within the topsoil increased from 1.9 for the most labile to 3.8 for the least labile respired SOM, whereas corresponding Q₁₀ values for the subsoil did not show this trend (Q₁₀ between 1.4 and 0.9). These results indicate the existence of a limiting factor that attenuates the intrinsic effect of SOM quality on Q₁₀ in the subsoil. A parallel incubation experiment of ¹³C‐labeled plant material added to top‐ and subsoil showed that decomposition of an unprotected C substrate of equal quality responds similarly to temperature changes in top‐ and subsoil. This further confirms that the attenuating effect on Q₁₀ in the subsoil originates from SOM protection rather than from microbial properties or other nutrient limitations. In conclusion, we found experimental evidence that SOM protection can attenuate the intrinsic Q₁₀ of SOM decomposition.     

Growth dynamics and biomass allocation of Eleocharis sphacelata at different water depths: observations, modeling, and applications

Imbalanced biomass allocation patterns in emergent aquatic plants to above and below-ground structures as a response to climatic variations and water depth were investigated on the basis of observation of three stable homogeneous populations established under different water regimes and climatic environments in Goulburn and Ourimbah, New South Wales, Australia, from August 2003 to December 2004. The growth of shoots depended on water inundation-drawdown patterns and climatic variations. Shoot density was greater in shallow water but with shorter shoot length and less maximum above-ground biomass density than for plant stands in deep water. Deep-water populations attained higher below-ground biomass with higher above to below-ground biomass ratio than for the shallow-water population. Translocation of carbohydrate reserves between above and below-ground organs in deep-water populations were mostly downward throughout the year whereas the depletion–recharge pattern varied seasonally in shallow water populations. Shoots of deep-water populations grew year-round whereas in shallow water shoots died off after recession of the water level with no re-growth afterward, showing that Eleocharis sphacelata is better adapted to deep water and is stressed under shallow-water conditions. A mathematical model was formulated to describe the growth patterns of E. sphacelata and subsequently to predict the effect of water depth on production. Model simulations are in satisfactory agreement with observed patterns of growth. The model also predicts that maximum production decreases sharply with increasing water depth.     

Soil organic carbon changes as influenced by agricultural land use and management: a case study in Yanhuai Basin, Beijing, China

The effects of agricultural land use and management practices on soil organic carbon (SOC) are of great concern. In this study, SOC changes were investigated in sandy loam soils (Ustochrepts, USDA Soil Taxonomy) under orchard, vegetable, corn (Zea maize L.), and soybean (Glycine max L.) cultivation in northern China. The corn fields were further classified into three categories based on their inputs, i.e. high-input, mid-input, and low-input corn fields. In April 2005, a total of 197 soil samples were collected from 42 soil sites within 100 cm soil depth in Yanhuai Basin, Beijing, China. SOC contents were determined using rapid dichromate oxidation, and ANOVA statistical analysis was used to test the significances between land use and management practices at p<0.05. The results showed that: (1) the effects of land use and management practices on SOC primarily occurred within the topsoil (0–25 cm), and the SOC contents sharply decreased with the increase in soil depth. (2) SOC content and density values of orchard, vegetable, and high-input corn fields were higher than those of soybean, mid- and low-input corn fields.     

不同农业土地利用方式和管理对土壤有机碳的影响 ——以北京市延庆盆地为例

自20世纪80年代以来,我国农业土地利用方式和农田管理发生了巨大变化,由此引起的土壤有机碳（SOC）含量、密度及其垂直分布发生了相应的变化,研究不同土地利用方式和管理对土壤有机碳的影响对于探讨农田生态系统的固碳作用具有重要的意义.以北京市延怀盆地为典型研究地区,选择6种农业土地利用和管理模式,共计42块样地,在1m深土体内分层采集197个土壤样品.研究结果表明：（1） 不同农业土地利用和管理方式对SOC含量的影响主要发生在0～25 cm土层中,剖面中SOC含量自上向下明显降低.（2） 通过对6种土地利用和管理方式下土壤SOC含量进行比较,结果发现果园和高投入的玉米地土壤在0～100 cm土层中SOC含量均较高,变化范围分别为4.16～10.00 g kg^-1和4.73～9.31 g kg^-1; 菜地土壤在0～40 cm土层中SOC含量较高,变化范围为6.42～9.67 g kg^-1;大豆地、中、低投入玉米地土壤在0～100 cm土层中SOC含量较低,变化范围分别为3.27～7.73 g kg^-1、3.14～8.33 g kg^-1和1.83～7.67 g kg^-1. （3） 不同农业土地利用方式对SOC密度影响的趋势与对SOC含量影响的趋势基本一致,在0～100 cm土壤中,SOC密度的顺序为果园＞菜地＞高投入玉米地＞中投入玉米地＞大豆地＞低投入玉米地,变化范围为4.15～8.22 kg m^-2.     

光照、盐分和埋深对无芒隐子草和条叶车前种子萌发的影响

光照、盐分和埋深对无芒隐子草(Cleistogenes songorica)和条叶车前(Plantago lessingii)种子萌发的影响研究结果显示,无芒隐子草和条叶车前种子为萌发需光性种子。随着盐(NaCl)浓度的增加,2种植物种子的发芽率呈直线下降趋势(P<0.01),但以条叶车前下降较为缓慢。当盐分浓度为0.4 mol.L-1时,2种植物种子皆不能萌发。低浓度的盐分促进胚根的生长,高浓度则表现为抑制作用;盐分对胚芽的生长则一直起抑制作用。2种植物种子发芽率随埋深的增加而减小,当埋深>2 cm时不能萌发。