CO2 emissions from land‐use change affected more by nitrogen cycle,than by the choice of land‐cover data

The high uncertainty in land‐based CO₂ fluxes estimates is thought to be mainly due to uncertainty in not only quantifying historical changes among forests, croplands, and grassland, but also due to different processes included in calculation methods. Inclusion of a nitrogen (N) cycle in models is fairly recent and strongly affects carbon (C) fluxes. In this study, for the first time, we use a model with C and N dynamics with three distinct historical reconstructions of land‐use and land‐use change (LULUC) to quantify LULUC emissions and uncertainty that includes the integrated effects of not only climate and CO₂ but also N. The modeled global average emissions including N dynamics for the 1980s, 1990s, and 2000–2005 were 1.8 ± 0.2, 1.7 ± 0.2, and 1.4 ± 0.2 GtC yr^?1, respectively, (mean and range across LULUC data sets). The emissions from tropics were 0.8 ± 0.2, 0.8 ± 0.2, and 0.7 ± 0.3 GtC yr^?1, and the non tropics were 1.1 ± 0.5, 0.9 ± 0.2, and 0.7 ± 0.1 GtC yr^?1. Compared to previous studies that did not include N dynamics, modeled net LULUC emissions were higher, particularly in the non tropics. In the model, N limitation reduces regrowth rates of vegetation in temperate areas resulting in higher net emissions. Our results indicate that exclusion of N dynamics leads to an underestimation of LULUC emissions by around 70% in the non tropics, 10% in the tropics, and 40% globally in the 1990s. The differences due to inclusion/exclusion of the N cycle of 0.1 GtC yr^?1 in the tropics, 0.6 GtC yr^?1 in the non tropics, and 0.7 GtC yr^?1 globally (mean across land‐cover data sets) in the 1990s were greater than differences due to the land‐cover data in the non tropics and globally (0.2 GtC yr^?1). While land‐cover information is improving with satellite and inventory data, this study indicates the importance of accounting for different processes, in particular the N cycle.     

Evaluating the effects of terrestrial ecosystems, climate and carbon dioxide on weathering over geological time: a global-scale process-based approach

Global weathering of calcium and magnesium silicate rocks provides the long-term sink for atmospheric carbon dioxide (CO(2)) on a timescale of millions of years by causing precipitation of calcium carbonates on the seafloor. Catchment-scale field studies consistently indicate that vegetation increases silicate rock weathering, but incorporating the effects of trees and fungal symbionts into geochemical carbon cycle models has relied upon simple empirical scaling functions. Here, we describe the development and application of a process-based approach to deriving quantitative estimates of weathering by plant roots, associated symbiotic mycorrhizal fungi and climate. Our approach accounts for the influence of terrestrial primary productivity via nutrient uptake on soil chemistry and mineral weathering, driven by simulations using a dynamic global vegetation model coupled to an ocean-atmosphere general circulation model of the Earth's climate. The strategy is successfully validated against observations of weathering in watersheds around the world, indicating that it may have some utility when extrapolated into the past. When applied to a suite of six global simulations from 215 to 50 Ma, we find significantly larger effects over the past 220 Myr relative to the present day. Vegetation and mycorrhizal fungi enhanced climate-driven weathering by a factor of up to 2. Overall, we demonstrate a more realistic process-based treatment of plant fungal-geosphere interactions at the global scale, which constitutes a first step towards developing 'next-generation' geochemical models.     

Luteal blood flow is a more appropriate indicator for luteal function during the bovine estrous cycle than luteal size

The objective of this study was to assess the reliability of luteal blood flow (LBF) as recorded by color Doppler sonography to monitor luteal function during the estrous cycle of dairy cows and to compare the results with that for the established criterion luteal size (LS) as determined by B-mode sonography. In total, 14 consecutive sonographic examinations were carried out in 10 synchronized lactating Holstein-Friesian cows (Bos taurus) on Days 4, 5, 6, 7, 8, 10, 12, 14, 16, -5, -4, -3, -2, -1 of the estrous cycle (Day 1 = ovulation). Plasma progesterone concentrations in venous blood (P₄) were quantified by enzyme immunoassay. Luteal size was determined by sonographic measurement of the maximal cross-sectional area of the corpus luteum (CL). Luteal blood supply was estimated by calculating the maximum colored area of the CL from power Doppler sonographic images. Luteal size doubled during the luteal growth phase (until Day 7) and remained at this level during the luteal static phase (Day 8 to 16) before decreasing rather slowly during luteal regression (Days -5 to -1). Luteal blood flow doubled during the growth phase, doubled furthermore during the static phase, and decreased rapidly during luteal regression. Thus, LBF values represented highly reliable predictors of luteal status. Luteal blood flow predicted reliably a P₄ > 1.0 ng/mL by reaching only 35% of the maximal values, whereas LS had to exceed 60% of the maximal values to indicate reliably a functional CL. It is concluded that LBF reflected luteal function better than LS specifically during luteal regression.     

Mechanisms for the increase in phosphorus uptake of waterlogged plants: soil phosphorus availability, root morphology and uptake kinetics

Waterlogging frequently reduces plant biomass allocation to roots. This response may result in a variety of alterations in mineral nutrition, which range from a proportional lowering of whole-plant nutrient concentration as a result of unchanged uptake per unit of root biomass, to a maintenance of nutrient concentration by means of an increase in uptake per unit of root biomass. The first objective of this paper was to test these two alternative hypothetical responses. In a pot experiment, we evaluated how plant P concentration of Paspalum dilatatum, (a waterlogging-tolerant grass from the Flooding Pampa, Argentina) was affected by waterlogging and P supply and how this related to changes in root-shoot ratio. Under both soil P levels waterlogging reduced root-shoot ratios, but did not reduce P concentration. Thus, uptake of P per unit of root biomass increased under waterlogging. Our second objective was to test three non-exclusive hypotheses about potential mechanisms for this increase in P uptake. We hypothesized that the greater P uptake per unit of root biomass was a consequence of: (1) an increase in soil P availability induced by waterlogging; (2) a change in root morphology, and/or (3) an increase in the intrinsic uptake capacity of each unit of root biomass. To test these hypotheses we evaluated (1) changes in P availability induced by waterlogging; (2) specific root length of waterlogged and control plants, and (3) P uptake kinetics in excised roots from waterlogged and control plants. The results supported the three hypotheses. Soil P avail-ability was higher during waterlogging periods, roots of waterlogged plants showed a morphology more favorable to nutrient uptake (finer roots) and these roots showed a higher physiological capacity to absorb P. The results suggest that both soil and plant mechanisms contributed to compensate, in terms of P nutrition, for the reduction in allocation to root growth. The rapid transformation of the P uptake system is likely an advantage for plants inhabiting frequently flooded environments with low P fertility, like the Flooding Pampa. This advantage would be one of the reasons for the increased relative abundance of P. dilatatum in the community after waterlogging periods. Received: 15 February 1997 / Accepted: 20 May 1997     

杭州市公交车油改电项目碳排放效益核算

以减少碳排放为核心的应对气候变化行动已成为全球趋势,中国政府积极践行减少碳排放的国际承诺,出台多项鼓励新能源的政策措施,其中包括对新能源产业的补偿以及将燃油汽车改装为电动汽车。但是这些政策的实施效果并不太清楚。举例来说,煤电为主的供电类型极大削弱了碳减排的效果,充电桩等配套基础设施建设和旧车报废等过程还会产生额外碳排放,不同城市之间的这些情况差别也较大。因此,城市层面生命周期尺度上的电动车碳减排效果尚未明确。基于生命周期理论,以杭州市为例,在构建公交车生命周期模型下分别核算纯电动和柴油车生命周期碳排放量,并在基准情景、低碳情景和强化低碳情景下进行公交车油改电碳排模拟。研究结果表明:(1)杭州市单辆纯电动和柴油公交车生命周期CO2排放量分别为1103.237t和1401.319t,减排比例达21.27%。其中,电力生产约占纯电动车生命周期碳排量74.10%,柴油生产与消耗约占柴油车生命周期碳排量86.96%;(2)目前杭州市在营运的2312辆纯电动公交车生命周期内(13年)碳减排总量约达到68.917万t,年均5.301万t;(3)在油改电过程中,纯电动公交车需运行约3.5年后才能相对柴油公交车真正起到碳减排效果;(4)在不同新煤电技术及能源结构优化下,2020、2035和2050年杭州市公交车油改电项目每辆车碳减排量将达到354.071—884.339t,年均27.236—68.026t,减排比例25.27%—63.11%,且2050年强化情景下纯公交车生命周期碳排量仅为当前纯电动公交车和柴油公交车的46.86%和36.89%,潜在碳减排效益显著。     

Fire and habitat management for a mycophagous marsupial,the Tasmanian bettong Bettongia gaimardi

Abstract The Tasmanian bettong, Bettongia gaimardi, is a mycophagous marsupial that occurs in fire-prone dry sclerophyll forests. Previous studies have demonstrated that some of the hypogeous fungi on which it feeds become abundant soon after fire, and have suggested that it might depend on regular burning of its habitat. The longer-term effects of burning on B. gaimardi and its food supply were evaluated by comparing six sites, matched for soil, vegetation and climate, in southeastern Tasmania that had been left unburnt for periods ranging from 1 to 50 years. At each site, the density of B. gaimardi diggings was measured and sporocarps of hypogeous fungi were surveyed. Abundance of hypogeous sporo-carps was low at sites 2 years or less post-fire, but was high at sites 4 years and more post-fire. Species richness was similarly low at recently burnt sites, an effect that was due to the absence of many shallow-fruiting taxa. All species (with one exception) present at recently burnt sites were also present in long-unburnt sites. Densities of B. gaimardi diggings were highest at a very recently burnt (<1 year) site and at a site left unburnt for 10 years. These trends suggest that a high frequency of burning may be unfavourable to B. gaimardi in the forest type investigated in this study.     

高寒矮嵩草草甸大气-土壤-植被-动物系统碳素储量及碳素循环

对高寒矮嵩草草甸生态系统中大气 -土壤 -植被 -动物分室碳素储量及碳素循环进行了研究 ,结果表明 ,草毡寒冻雏形土土壤库 0～ 30 cm碳素储量为 2 4 7.30 t C/ hm2 。土壤 CO2 平均释放速率 70 .94± 54.76kg/ (hm2· d) ,年释放量为 6.630 t C/ (hm2·a) ,比退化草地 4.62 0 t C/ (hm2·a)释放量高。植物包括根系总固碳量为 4.648t C/ (hm2· a) ,动物亚系统中 ,藏系绵羊个体同化的碳素为 7.562 kg C/ (hm2· a) (成年羊 ) ,作为畜产品迁出生态系统。生态系统初级生产固碳量占每年土壤 CO2 释放量的 70 .1 6% ,占生长季土壤 CO2 释放量的 96.43% ,退化草地土壤 CO2 释放量比初级生产固碳量要低。认为高寒矮嵩草草甸生态系统土壤是大气温室气体 CO2 的小的排放源。     

Estimation of photosynthesis and calcification rates at a fringing reef by accounting for diurnal variations and the zonation of coral reef communities on reef flat and slope: a case study for the Shiraho reef, Ishigaki Island, southwest Japan

Seven coral reef communities were defined on Shiraho fringing reef, Ishigaki Island, Japan. Net photosynthesis and calcification rates were measured by in situ incubations at 10 sites that included six of the defined communities, and which occupied most of the area on the reef flat and slope. Net photosynthesis on the reef flat was positive overall, but the reef flat acts as a source for atmospheric CO₂, because the measured calcification/photosynthesis ratio of 2.5 is greater than the critical ratio of 1.67. Net photosynthesis on the reef slope was negative. Almost all excess organic production from the reef flat is expected to be effused to the outer reef and consumed by the communities there. Therefore, the total net organic production of the whole reef system is probably almost zero and the whole reef system also acts as a source for atmospheric CO₂. Net calcification rates of the reef slope corals were much lower than those of the branching corals. The accumulation rate of the former was approximately 0.5 m kyr⁻¹ and of the latter was ~0.7–5 m kyr⁻¹. Consequently, reef slope corals could not grow fast enough to keep up with or catch up to rising sea levels during the Holocene. On the other hand, the branching corals grow fast enough to keep up with this rising sea level. Therefore, a transition between early Holocene and present-day reef communities is expected. Branching coral communities would have dominated while reef growth kept pace with sea level rise, and the reef was constructed with a branching coral framework. Then, the outside of this framework was covered and built up by reef slope corals and present-day reefs were constructed.     

A seasonal study of the carbon content of planktonic naked amoebae in the Hudson Estuary and in a productive freshwater pond with comparative data for ciliates

The total carbon contents of gymnamoebae and ciliates, dwelling in the water column of the Hudson Estuary and a highly productive freshwater pond, were monitored during a 7-month period from April through October 2006. The carbon contents of the gymnamoebae and the ciliates were greater in the pond compared with the estuary, and carbon contents of gymnamoebae were greater in the spring and autumn in both locations than those of ciliates. Given the global distribution of gymnamoebae, these results suggest that greater attention should be given to the potential role of gymnamoebae in microbial food webs.     

Spatial distribution, connectivity, and the influence of scale: habitat availability for the endangered Mona Island rock iguana

The Caribbean region is one of the five leading biodiversity hotspots in the world. Analysis of the spatial structure of critical habitats and how it affects endemic species in this region is essential baseline information for biodiversity monitoring and management. We quantified and evaluated the spatial structure and connectivity of depression forests on Mona Island and their potential impact on Mona Island rock iguana habitat, as a framework to assess spatial distribution, connectivity, and the issue of scale in small and widely dispersed habitats. Using IKONOS imagery, we mapped and delineated depression forests at four different scales (minimum mapping units: <100, 100, 500, and 1,000 m), and calculated landscape metrics describing their spatial structure, and connectivity, for each map resolution. Our approach resulted in a more detailed map than previously described maps, providing better information on habitat connectivity for iguanas. The comparison of the island landscape mapped at different scales provided evidence on how changing scales affect the output of spatial metrics and may have a significant impact when planning decisions and assigning conservation priorities. It also highlighted the importance of adequate ecological scales when addressing landscape management and conservation priorities. The analysis of landscapes at multiple scales provided a mechanism to evaluate the role of patch detection and its effect on the interpretation of connectivity and spatial structure of suitable areas for species with small and widely dispersed habitats. These methodologies can be applied other species, in different environments, with similar limitations related to connectivity and habitat availability.     

De novo lipogenesis in the liver in health and disease: more than just a shunting yard for glucose

Hepatic de novo lipogenesis (DNL) is the biochemical process of synthesising fatty acids from acetyl‐CoA subunits that are produced from a number of different pathways within the cell, most commonly carbohydrate catabolism. In addition to glucose which most commonly supplies carbon units for DNL, fructose is also a profoundly lipogenic substrate that can drive DNL, important when considering the increasing use of fructose in corn syrup as a sweetener. In the context of disease, DNL is thought to contribute to the pathogenesis of non‐alcoholic fatty liver disease, a common condition often associated with the metabolic syndrome and consequent insulin resistance. Whether DNL plays a significant role in the pathogenesis of insulin resistance is yet to be fully elucidated, but it may be that the prevalent products of this synthetic process induce some aspect of hepatic insulin resistance.     

PP2A: more than a reset switch to activate pRB proteins during the cell cycle and in response to signaling cues

In their active hypophosphorylated state, members of the retinoblastoma family of pocket proteins negatively regulate cell cycle progression at least in part by repressing expression of E2F-dependent genes. Mitogen-dependent activation of G1 and G1/S Cyclin Dependent Kinases (CDKs) results in coordinated hyperphosphorylation and inactivation of these proteins, which no longer bind and repress E2Fs. S and G2/M CDKs maintain pocket protein hyperphosphorylated through the end of mitosis. The inactivating action of inducible CDKs is opposed by the Ser/Thr protein phosphatases PP2A and PP1. Various trimeric PP2A holoenzymes have been implicated in dephosphorylation of pocket proteins in response to specific cellular signals and stresses or as part of an equilibrium with CDKs throughout the cell cycle. PP1 has specifically been implicated in dephosphorylation of pRB in late mitosis and early G1. This review is particularly focused on the emerging role of PP2A as a major hub for integration of growth suppressor signals that require rapid inactivation of pocket proteins. Of note, activation of particular PP2A holoenzymes triggers differential activation of pocket proteins in the presence of active CDKs.     

A sequence stratigraphical model for the Late Ludfordian (Silurian) of Gotland,Sweden: implications for timing between changes in sea level,palaeoecology, and the global carbon cycle

This paper investigates a time interval within the Late Ludfordian (Late Silurian), involving changes in faunal composition (the Lau Event), a major positive carbon isotope excursion (CIE), and contemporaneous sea-level changes in remote palaeo-basins. Based on the Silurian strata of Gotland (Sweden), we integrate sequence stratigraphy, carbon isotope stratigraphy, and platform-scale palaeoecological changes associated with this turbulent time period in Earth history. Three depositional sequences (sequences Nos. 1–3), including two separate periods of forced regression (falling stage systems tracts, FSSTs) are identified from outcrop and drillcore studies. The sequence stratigraphical framework is interpreted to reflect glacio-eustatic sea-level changes. The CIE starts at the onset of the initial FSST (sequence No. 1), just below the last appearance datum of the conodont Polygnathoides siluricus. The values increase through the ensuing lowstand and transgressive systems tracts (LST and TST) of sequence No. 2 and peak in the following highstand systems tract (HST). A second forced regression (FSST of sequence No. 2) took place in the lower Ozarkodina snajdri Zone. δ¹³C data are scarce from these siliciclastic strata, but inferably remain high. The δ¹³C values increase within the LST and earliest TST of sequence No. 3, before a decreasing trend starts within the early TST. δ¹³C values return to pre-excursion levels within the ensuing HST. The CIE is closely associated with an increase in stromatolites (mats and oncoids) across a wide range of depths and sedimentary environments, and correlations to other basins indicate a global increase in cyanobacterial activity. A drastic decline in level-bottom benthic faunas during the FSST of sequence No. 2 is, however, interpreted as a local response to the progradation of a delta complex (the Burgsvik Sandstone). Biological carbonate production replenishes rapidly within the TST of sequence No. 3, succeeding a thin LST dominated by reworked siliciclastics and chemically precipitated carbonates (ooids). The detailed relationship between the CIE and sea-level change presented herein is not fully consistent with previous reports on the CIEs associated with the lower Silurian Ireviken and Mulde events, respectively. Based on our facies analysis and sequence stratigraphical interpretation, two main mechanisms are suggested as responsible for the Late Ludfordian CIE: (1) a change in the riverine C-weathering flux towards the ¹³C end member following glacio-eustatically induced subaerial exposure of carbonate platforms throughout the tropics, and, (2) increased photosynthetic activity by benthic cyanobacteria exaggerating the δ¹³C values of precipitated carbonates.     

The role of interannual,seasonal, and synoptic climate on the carbon isotope ratio of ecosystem respiration at a semiarid woodland

The terrestrial carbon cycle is influenced by environmental variability at scales ranging from diurnal to interannual. Here, we present 5‐years of growing season (day 131–275) observations of the carbon isotope ratio of ecosystem respiration (δ¹³C_R) from a semiarid woodland. This ecosystem has a large necromass component resulting from 97%Pinus edulis mortality in 2002, is dominated by drought‐tolerant Juniperus monosperma trees, and experiences large variability in the timing and intensity of seasonal and synoptic water availability. Mean growing season δ¹³C_R was remarkably invariant (?23.57±0.4‰), with the exception of particularly enriched δ¹³C_R in 2006 following a winter with anomalously low snowfall. δ¹³C_R was strongly coupled to climate during premonsoon periods (～May to June), including fast (≤2 days) responses to changes in crown‐level stomatal conductance (G_c) and vapor pressure deficit (vpd) following rain pulses. In contrast, δ¹³C_R was relatively decoupled from G_c and environmental drivers during monsoon and postmonsoon periods (July–August and September, respectively), exhibiting only infrequent couplings of δ¹³C_R to vpd and soil water content (SWC) with longer lags (～8 days) and variable response slopes (both positive and negative). Notably, δ¹³C_R exhibited consistent dynamics after rainfall events, with depleted δ¹³C_R occurring within 1 h, progressive hourly δ¹³C_R enrichment over the remainder of the night, and net δ¹³C_R depletions over the multiple nights postevent in monsoon and postmonsoon periods. Overall this ecosystem demonstrated strong dependence of δ¹³C_R on precipitation, with an apparent dominance by the autotrophic δ¹³C signal in premonsoon periods when deep soil moisture is abundant and surface soil moisture is low, and weaker coupling during monsoonal periods consistent with increasing heterotrophic dominance when deep soil moisture has declined and surface moisture is variable.     

PP2A: more than a reset switch to activate pRB proteins during the cell cycle and in response to signaling cues

In their active hypophosphorylated state, members of the retinoblastoma family of pocket proteins negatively regulate cell cycle progression at least in part by repressing expression of E2F-dependent genes. Mitogen-dependent activation of G1 and G1/S Cyclin Dependent Kinases (CDKs) results in coordinated hyperphosphorylation and inactivation of these proteins, which no longer bind and repress E2Fs. S and G2/M CDKs maintain pocket protein hyperphosphorylated through the end of mitosis. The inactivating action of inducible CDKs is opposed by the Ser/Thr protein phosphatases PP2A and PP1. Various trimeric PP2A holoenzymes have been implicated in dephosphorylation of pocket proteins in response to specific cellular signals and stresses or as part of an equilibrium with CDKs throughout the cell cycle. PP1 has specifically been implicated in dephosphorylation of pRB in late mitosis and early G1. This review is particularly focused on the emerging role of PP2A as a major hub for integration of growth suppressor signals that require rapid inactivation of pocket proteins. Of note, activation of particular PP2A holoenzymes triggers differential activation of pocket proteins in the presence of active CDKs.     

黄土丘陵区刺槐、辽东栎林地土壤碳、氮、磷生态化学计量特征

黄土高原中部的丘陵沟壑区位于半湿润、半干旱气候带,生态环境脆弱,水土流失严重,植被恢复是该地区水土保持与生态重建的重要措施。辽东栎天然次生林和刺槐人工林是该地区典型的森林植被类型。以黄土丘陵森林分布区边缘的两种主要森林类型为对象,通过采集林地不同深度土壤样品,对比分析两种林地土壤中碳、氮、磷含量的计量关系及垂直分布特征,旨在探明该区域土壤化学计量特征及主要影响因素。结果表明:(1)在两种林地类型中,土壤有机碳与全碳含量呈正相关关系,两种林地可用同一曲线进行拟合,说明特定土壤类型在同一区域其有机碳和无机碳相对含量基本稳定。(2)土壤有机碳与全氮比值在10左右,在不同土层深度无明显变化;而土壤全碳与全氮比值则随土壤深度的增加而增加,超过1 m以后呈现饱和曲线的变化趋势。(3)土壤氮磷比随土壤深度的增加呈幂次型降低。