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排序方式： 共有903条查询结果，搜索用时 19 毫秒
91.
Fiona L. Gill Jürgen Hummel A. Reza Sharifi Alexandra P. Lee Barry H. Lomax 《Palaeontology》2018,61(5):647-658
A major uncertainty in estimating energy budgets and population densities of extinct animals is the carrying capacity of their ecosystems, constrained by net primary productivity (NPP) and its digestible energy content. The hypothesis that increases in NPP due to elevated atmospheric CO2 contributed to the unparalleled size of the sauropods has recently been rejected, based on modern studies on herbivorous insects that imply a general, negative correlation of diet quality and increasing CO2. However, the nutritional value of plants grown under elevated CO2 levels might be very different for vertebrate megaherbivores than for insects. Here we show plant species‐specific responses in metabolizable energy and nitrogen content, equivalent to a two‐fold variation in daily food intake estimates for a typical sauropod, for dinosaur food plant analogues grown under CO2 concentrations spanning estimates for Mesozoic atmospheric concentrations. Our results potentially rebut the hypothesis that constraints on sauropod diet quality were driven by Mesozoic CO2 concentration. 相似文献
92.
The incomplete combustion of vegetation and dead organic matter by landscape fires creates recalcitrant pyrogenic carbon (PyC), which could be consequential for the global carbon budget if changes in fire regime, climate, and atmospheric CO2 were to substantially affect gains and losses of PyC on land and in oceans. Here, we included global PyC cycling in a coupled climate–carbon model to assess the role of PyC in historical and future simulations, accounting for uncertainties through five sets of parameter estimates. We obtained year‐2000 global stocks of (Central estimate, likely uncertainty range in parentheses) 86 (11–154), 47 (2–64), and 1129 (90–5892) Pg C for terrestrial residual PyC (RPyC), marine dissolved PyC, and marine particulate PyC, respectively. PyC cycling decreased atmospheric CO2 only slightly between 1751 and 2000 (by 0.8 Pg C for the Central estimate) as PyC‐related fluxes changed little over the period. For 2000 to 2300, we combined Representative Concentration Pathways (RCPs) 4.5 and 8.5 with stable or continuously increasing future fire frequencies. For the increasing future fire regime, the production of new RPyC generally outpaced the warming‐induced accelerated loss of existing RPyC, so that PyC cycling decreased atmospheric CO2 between 2000 and 2300 for most estimates (by 4–8 Pg C for Central). For the stable fire regime, however, PyC cycling usually increased atmospheric CO2 (by 1–9 Pg C for Central), and only the most extreme choice of parameters maximizing PyC production and minimizing PyC decomposition led to atmospheric CO2 decreases under RCPs 4.5 and 8.5 (by 5–8 Pg C). Our results suggest that PyC cycling will likely reduce the future increase in atmospheric CO2 if landscape fires become much more frequent; however, in the absence of a substantial increase in fire frequency, PyC cycling might contribute to, rather than mitigate, the future increase in atmospheric CO2. 相似文献
93.
The effect of wind speed and distance from the source on the male response of the aphid parasitoid, Aphidius ervi (Hymenoptera: Aphidiidae), to a pheromone source was studied in a wind tunnel. The number of males taking flight, entering
the plume and successfully reaching the source, decreased at wind speeds >50 cm/s. Furthermore, the proportion of those attempting
upwind flight that fell to the ground increased with increasing wind speed. In contrast, distance from the source had no significant
effect on any of the parameters examined. While male flight behavior was significantly reduced at 70 cm/s, some males walked
to the source when there was a bridge connecting the pheromone source and the release platform. This suggests that ambulatory
behavior could be a significant component of male mate searching in A. ervi when wind conditions are too strong for upwind flight. The possible effects of variation in atmospheric pressure on male
flight behavior to the long distance pheromone, as well as to the short distance one, were also investigated. No significant
effects of atmospheric pressure were observed. These findings differ significantly from those previously reported for another
aphid parasitoid, A. nigripes, and the reasons for such differences are discussed. 相似文献
94.
Irena F. Creed Ann‐Kristin Bergström Charles G. Trick Nancy B. Grimm Dag O. Hessen Jan Karlsson Karen A. Kidd Emma Kritzberg Diane M. McKnight Erika C. Freeman Oscar E. Senar Agneta Andersson Jenny Ask Martin Berggren Mehdi Cherif Reiner Giesler Erin R. Hotchkiss Pirkko Kortelainen Monica M. Palta Tobias Vrede Gesa A. Weyhenmeyer 《Global Change Biology》2018,24(8):3692-3714
Northern ecosystems are experiencing some of the most dramatic impacts of global change on Earth. Rising temperatures, hydrological intensification, changes in atmospheric acid deposition and associated acidification recovery, and changes in vegetative cover are resulting in fundamental changes in terrestrial–aquatic biogeochemical linkages. The effects of global change are readily observed in alterations in the supply of dissolved organic matter (DOM)—the messenger between terrestrial and lake ecosystems—with potentially profound effects on the structure and function of lakes. Northern terrestrial ecosystems contain substantial stores of organic matter and filter or funnel DOM, affecting the timing and magnitude of DOM delivery to surface waters. This terrestrial DOM is processed in streams, rivers, and lakes, ultimately shifting its composition, stoichiometry, and bioavailability. Here, we explore the potential consequences of these global change‐driven effects for lake food webs at northern latitudes. Notably, we provide evidence that increased allochthonous DOM supply to lakes is overwhelming increased autochthonous DOM supply that potentially results from earlier ice‐out and a longer growing season. Furthermore, we assess the potential implications of this shift for the nutritional quality of autotrophs in terms of their stoichiometry, fatty acid composition, toxin production, and methylmercury concentration, and therefore, contaminant transfer through the food web. We conclude that global change in northern regions leads not only to reduced primary productivity but also to nutritionally poorer lake food webs, with discernible consequences for the trophic web to fish and humans. 相似文献
95.
《植物生态学报》2016,40(7):686
Aims Our objectives were to explore the effects of simulated nitrogen deposition on leaf traits and ecological stoichiometry characteristics of common species in natural Pinus tabuliformis forests.
Methods We conducted the experiment of nitrogen (N) addition from 2009 to 2013 in the natural Pinus tabuliformis forests in Taiyue Mountain, Shanxi, China. The levels of N addition were 0 (control), 50 (low-N), 100 (medium-N) and 150 (high-N) kg·hm-2·a-1, respectively. Eleven common plant species in 12 20 m × 20 m plots were selected, including Pinus tabuliformis, Quercus mongolica, Acer ginnala, Corylus mandshurica, Cornus bretschneideri, Spiraea salicifolia, Lonicera maackii, Carex callitrichos, Diarrhena mandshurica, Anemone tomentosa, and Polygonatum odoratum. Nine leaf traits were measured, including leaf thickness (LT), specific leaf area (SLA), leaf dry matter content (LDMC), leaf nitrogen content (LNC), leaf phosphorus content (LPC), and other four.
Important findings We found that: 1) LT and SLA of Polygonatum odoratum significantly differed among four levels of N addition. Leaf area (LA) and LDMC of several species, such as Spiraea salicifolia, had significant difference among the N addition concentration. LNC of all species, chlorophyll content (CC) and LPC of most species increased significantly with the addition of N. Leaf N:P of 9 species varied significantly, and leaves with different types and ages showed different responses to N addition. 2) Leaf traits were significantly correlated with each other. For instance, SLA was significantly positively correlated with LNC and LPC. In contrast LT was negatively connected with LNC and LPC. In addition, the degree of correlation changed with the level of N addition. 3) The pattern of species distribution in leaf trait space was consistent with the prediction from the theory of Leaf Economic Spectrum (LES). N addition drove species moving along axis 1 in the trait space, and propelled them towards different directions along axis 2, which indicated that these species tended to take the “fast investment-return” strategy. These results suggested that with the change of environmental conditions, plants changed their survival strategy and adjusted resource allocation to maintain the stability of communities. This is the inherent characteristic of plants, thus the formation of LES did not depend on the environment change. 相似文献
Methods We conducted the experiment of nitrogen (N) addition from 2009 to 2013 in the natural Pinus tabuliformis forests in Taiyue Mountain, Shanxi, China. The levels of N addition were 0 (control), 50 (low-N), 100 (medium-N) and 150 (high-N) kg·hm-2·a-1, respectively. Eleven common plant species in 12 20 m × 20 m plots were selected, including Pinus tabuliformis, Quercus mongolica, Acer ginnala, Corylus mandshurica, Cornus bretschneideri, Spiraea salicifolia, Lonicera maackii, Carex callitrichos, Diarrhena mandshurica, Anemone tomentosa, and Polygonatum odoratum. Nine leaf traits were measured, including leaf thickness (LT), specific leaf area (SLA), leaf dry matter content (LDMC), leaf nitrogen content (LNC), leaf phosphorus content (LPC), and other four.
Important findings We found that: 1) LT and SLA of Polygonatum odoratum significantly differed among four levels of N addition. Leaf area (LA) and LDMC of several species, such as Spiraea salicifolia, had significant difference among the N addition concentration. LNC of all species, chlorophyll content (CC) and LPC of most species increased significantly with the addition of N. Leaf N:P of 9 species varied significantly, and leaves with different types and ages showed different responses to N addition. 2) Leaf traits were significantly correlated with each other. For instance, SLA was significantly positively correlated with LNC and LPC. In contrast LT was negatively connected with LNC and LPC. In addition, the degree of correlation changed with the level of N addition. 3) The pattern of species distribution in leaf trait space was consistent with the prediction from the theory of Leaf Economic Spectrum (LES). N addition drove species moving along axis 1 in the trait space, and propelled them towards different directions along axis 2, which indicated that these species tended to take the “fast investment-return” strategy. These results suggested that with the change of environmental conditions, plants changed their survival strategy and adjusted resource allocation to maintain the stability of communities. This is the inherent characteristic of plants, thus the formation of LES did not depend on the environment change. 相似文献
96.
97.
Timothy M. Lenton 《Global Change Biology》2001,7(6):613-629
The evolution of vascular plants and their spread across the land surface, beginning ～420 Ma, progressively increased the rate of weathering of phosphorus from rocks. This phosphorus supply promoted terrestrial and marine productivity and the burial of organic carbon, which has been the major source of O2 over geological timescales. Hence, it is predicted that the rise of plants led to an increase in the O2 content of the atmosphere from ～12 vol %, 570–400 Ma to its present level of ～21 vol % by ～340 Ma. Previous modelling studies suggest that O2 then rose to ～35 vol % ～300 Ma. Such high concentrations are difficult to reconcile with the known persistence of forests, because rising O2 increases the frequency and intensity of vegetation fires, tending to decrease biomass and cause ecological shifts toward faster regenerating ecosystems. Rising O2 also directly inhibits C3 photosynthetic carbon assimilation and increases the production of toxic reactive oxygen species in cells. These effects suppress plant‐induced phosphorus weathering and hence organic carbon burial, providing a sensitive negative feedback on O2. A revised model predicts that this mechanism could have regulated atmospheric O2 within the range 15–25 vol % for the last 350 million years. 相似文献
98.
Shilong Piao Zhuo Liu Yilong Wang Philippe Ciais Yitong Yao Shushi Peng Frédéric Chevallier Pierre Friedlingstein Ivan A. Janssens Josep Peñuelas Stephen Sitch Tao Wang 《Global Change Biology》2018,24(2):608-616
No consensus has yet been reached on the major factors driving the observed increase in the seasonal amplitude of atmospheric CO2 in the northern latitudes. In this study, we used atmospheric CO2 records from 26 northern hemisphere stations with a temporal coverage longer than 15 years, and an atmospheric transport model prescribed with net biome productivity (NBP) from an ensemble of nine terrestrial ecosystem models, to attribute change in the seasonal amplitude of atmospheric CO2. We found significant (p < .05) increases in seasonal peak‐to‐trough CO2 amplitude (AMPP‐T) at nine stations, and in trough‐to‐peak amplitude (AMPT‐P) at eight stations over the last three decades. Most of the stations that recorded increasing amplitudes are in Arctic and boreal regions (>50°N), consistent with previous observations that the amplitude increased faster at Barrow (Arctic) than at Mauna Loa (subtropics). The multi‐model ensemble mean (MMEM) shows that the response of ecosystem carbon cycling to rising CO2 concentration (eCO2) and climate change are dominant drivers of the increase in AMPP‐T and AMPT‐P in the high latitudes. At the Barrow station, the observed increase of AMPP‐T and AMPT‐P over the last 33 years is explained by eCO2 (39% and 42%) almost equally than by climate change (32% and 35%). The increased carbon losses during the months with a net carbon release in response to eCO2 are associated with higher ecosystem respiration due to the increase in carbon storage caused by eCO2 during carbon uptake period. Air‐sea CO2 fluxes (10% for AMPP‐T and 11% for AMPT‐P) and the impacts of land‐use change (marginally significant 3% for AMPP‐T and 4% for AMPT‐P) also contributed to the CO2 measured at Barrow, highlighting the role of these factors in regulating seasonal changes in the global carbon cycle. 相似文献
99.
潮间带海藻光合作用总是处于水生(高潮时)与气生(低潮时)两种连续变化的环境状态下进行.对汕头沿岸常见的潮间带海藻石莼(Ulva lactuca L.)在水生和气生不同状态下光合作用对无机碳的响应特性进行了比较研究.在水生状态下,现有海水中溶解性无机碳浓度能充分饱和(10 ℃和20 ℃时)或接近饱和(30 ℃时)石莼的光合作用;而在气生状态下,石莼光合作用受大气CO2浓度的限制,且这种限制作用在较高温度(20-30 ℃)下比在低温(10 ℃)下更严重.在10 ℃和20 ℃时,石莼在气生状态下比在水生状态下具有更高的碳饱和最大光合速率;而在30 ℃时,石莼在这两种状态下的碳饱和光合速率相似.石莼光合作用的Km (CO2)值在气生状态下比在水生状态下高;而在气生状态下石莼对CO2的表观光合导度远小于其在水生状态下的值.认为大气CO2浓度升高将通过促进石莼在气生状态下的光合作用而增加其初级生产力. 相似文献
100.
Ron J.G. Kaandorp Hubert B. VonhofCahuide Del Busto Frank P. Wesselingh Gerald M. GanssenAndrés E. Marmól Lidia Romero PittmanJan E. van Hinte 《Palaeogeography, Palaeoclimatology, Palaeoecology》2003,194(4):339-354
In a floodplain lake of the Amazon River near the city of Iquitos, northeastern Peru, a one-year monitoring experiment was conducted during which water samples and living bivalves (Anodontites trapesialis) were collected with the aim to investigate seasonal δ18O variation in and fractionation between bivalve aragonite and host water. Both host water and molluscan growth increments show more than 8‰ seasonal variation in δ18O. In the floodplain lake under study the δ18O variation of the water is controlled by contrasting dry and wet season evaporation-precipitation regimes. Molluscan δ18O appears to be in equilibrium with the host water. Although an approximately 4.0‰ offset occurs, δ13C records of water and bivalves are in good agreement, suggesting that both δ18O and δ13C of the shells of freshwater bivalve A. trapesialis are good recorders of (palaeo-)environmental conditions. The δ13C of Dissolved Inorganic Carbon (DIC) is governed by plant growth and/or by changes in aquatic chemistry, affecting the DIC pool. 相似文献