Phytoplankton decline in the eastern North Pacific transition zone associated with atmospheric blocking

Global climate change can significantly influence oceanic phytoplankton dynamics, and thus biogeochemical cycles and marine food webs. However, associative explanations based on the correlation between chlorophyll‐a concentration (Chl‐a) and climatic indices is inadequate to describe the mechanism of the connection between climate change, large‐scale atmospheric dynamics, and phytoplankton variability. Here, by analyzing multiple satellite observations of Chl‐a and atmospheric conditions from National Center for Environmental Prediction/National Center for Atmospheric Research reanalysis datasets, we show that high‐latitude atmospheric blocking events over Alaska are the primary drivers of the recent decline of Chl‐a in the eastern North Pacific transition zone. These blocking events were associated with the persistence of large‐scale atmosphere pressure fields that decreased westerly winds and southward Ekman transport over the subarctic ocean gyre. Reduced southward Ekman transport leads to reductions in nutrient availability to phytoplankton in the transition zone. The findings describe a previously unidentified climatic factor that contributed to the recent decline of phytoplankton in this region and propose a mechanism of the top‐down teleconnection between the high‐latitude atmospheric circulation anomalies and the subtropical oceanic primary productivity. The results also highlight the importance of understanding teleconnection among atmosphere–ocean interactions as a means to anticipate future climate change impacts on oceanic primary production.     

A kinetic comparison between E2P and the E2P-like state induced by a beryllium fluoride complex in the Na,K-ATPase. Interactions with Rb+

Metal-fluoride complexes have been used to induce E2P-like states with the aim of studying the events that occur during E2P hydrolysis in P-type ATPases. In the present work, we compared the E2P-like state induced by a beryllium fluoride complex (BeF_x) with the actual E2P state formed through backdoor phosphorylation of the Na,K-ATPase. Formation of E2P and E2P-like states were investigated employing the styryl dye RH421. We found that BeF_x is the only fluorinated phosphate analog that, like Pi, increases the RH421 fluorescence. The observed rate constant, k_obs, for the formation of E2P decreases with [Pi] whereas that of E2BeF_x increases with [BeF_x]. This might wrongly be taken as evidence of a mechanism where the binding of BeF_x induces a conformational transition. Here, we rather propose that, like for Pi, binding of BeF_x follows a conformational-selection mechanism, i.e. it binds to the E2 conformer forming a complex that is much more stable than E2P, as seen from its impaired capacity to return to E1 upon addition of Na⁺. Although E2P and E2BeF_x are able to form states with 2 occluded Rb⁺, both enzyme complexes differ in that the affinity for the binding and occlusion of the second Rb⁺ is much lower in E2BeF_x than in E2P. The higher rates of Rb⁺ occlusion and deocclusion observed for E2BeF_x, as compared to those observed for other E2P-like transition and product states suggest a more open access to the cation transport sites, supporting the idea that E2BeF_x mimics the E2P ground state.     

Discharge,legacy effects and nutrient availability as determinants of temporal patterns in biofilm metabolism and accrual in an arctic river

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Rapid adjustment of bird community compositions to local climatic variations and its functional consequences

The local spatial congruence between climate changes and community changes has rarely been studied over large areas. We proposed one of the first comprehensive frameworks tracking local changes in community composition related to climate changes. First, we investigated whether and how 12 years of changes in the local composition of bird communities were related to local climate variations. Then, we tested the consequences of this climate‐induced adjustment of communities on Grinnellian (habitat‐related) and Eltonian (function‐related) homogenization. A standardized protocol monitoring spatial and temporal trends of birds over France from 2001 to 2012 was used. For each plot and each year, we used the spring temperature and the spring precipitations and calculated three indices reflecting the thermal niche, the habitat specialization, and the functional originality of the species within a community. We then used a moving‐window approach to estimate the spatial distribution of the temporal trends in each of these indices and their congruency with local climatic variations. Temperature fluctuations and community dynamics were found to be highly variable in space, but their variations were finely congruent. More interestingly, the community adjustment to temperature variations was nonmonotonous. Instead, unexplained fluctuations in community composition were observed up to a certain threshold of climate change intensity, above which a change in community composition was observed. This shift corresponded to a significant decrease in the relative abundance of habitat specialists and functionally original species within communities, regardless of the direction of temperature change. The investigation of variations in climate and community responses appears to be a central step toward a better understanding of climate change effects on biodiversity. Our results suggest a fine‐scale and short‐term adjustment of community composition to temperature changes. Moreover, significant temperature variations seem to be responsible for both the Grinnellian and Eltonian aspects of functional homogenization.     

The type of competition modulates the ecophysiological response of grassland species to elevated CO2 and drought

The effects of elevated CO₂ and drought on ecophysiological parameters in grassland species have been examined, but few studies have investigated the effect of competition on those parameters under climate change conditions. The objective of this study was to determine the effect of elevated CO₂ and drought on the response of plant water relations, gas exchange, chlorophyll a fluorescence and aboveground biomass in four grassland species, as well as to assess whether the type of competition modulates that response. Elevated CO₂ in well‐watered conditions increased aboveground biomass by augmenting CO₂ assimilation. Drought reduced biomass by reducing CO₂ assimilation rate via stomatal limitation and, when drought was more severe, also non‐stomatal limitation. When plants were grown under the combined conditions of elevated CO₂ and drought, drought limitation observed under ambient CO₂ was reduced, permitting higher CO₂ assimilation and consequently reducing the observed decrease in aboveground biomass. The response to climate change was species‐specific and dependent on the type of competition. Thus, the response to elevated CO₂ in well‐watered grasses was higher in monoculture than in mixture, while it was higher in mixture compared to monoculture for forbs. On the other hand, forbs were more affected than grasses by drought in monoculture, while in mixture the negative effect of drought was higher in grasses than in forbs, due to a lower capacity to acquire water and mineral nutrients. These differences in species‐level growth responses to CO₂ and drought may lead to changes in the composition and biodiversity of the grassland plant community in future climate conditions.     

40年岷山地区白河自然保护区川金丝猴的生境格局动态

好的生境质量是野生动物生存和繁衍的必备条件,生境质量的变化将对动物的生存产生深远影响,定量客观的评估生境变迁过程显得尤为必要。川金丝猴作为我国一级保护动物,评定其生境质量变化过程有利于制定有效的保护措施。3S技术的不断发展与广泛应用为研究川金丝猴生境格局的动态变化提供了有利的工具。以岷山白河自然保护区为例,利用陆地资源卫星的MSS/TM/OLI遥感影像,并基于专家知识的决策树分类方法对遥感影像进行分类,获取了5个时期的覆被类型空间分布图;根据NDVI与郁闭度的相关性获取了研究区郁闭度的时空变化信息。然后,通过对野外观测数据的数理统计与空间分析,获取了川金丝猴的生活习性特征,并结合AHP方法构建了川金丝猴生境质量的评价体系,对5个时期的生境质量进行了评价,最后定量分析了40年来川金丝猴的生境格局的动态变化趋势。研究表明,近40年来白河自然保护区内及周边的生境经历了由良好到不断恶化,再到逐渐恢复的过程,其中最适宜和适宜生境呈现先降低后逐渐升高的趋势,而不适宜和勉强适宜则表现为先增加后减小的趋势。1975—1982年时段内,各生境等级变化剧烈,尤以最适宜和不适宜等级变化显著,生境质量整体呈恶化趋势;1982—1994年,各生境等级变化剧烈程度较前一时期有所缓和,生境质量得到较大改善,呈良性发展趋势;1994—2003年时段内,研究区内生境质量进一步改善,环境恶化状况得到了缓解;2003—2014年时间段内整体质量改善的速度明显减缓,生境质量达到平衡状态。除1975—2014时段外,前4个时段的各综合变化指标呈现递减趋势,前期生境等级变化剧烈,后期趋缓。气候变化和人为干扰为导致生境变化的主要因素,其中20世纪80年代生境变化与气候变化关系密切,而20世纪90年代之后人为干扰因素明显增加。研究有助于理解气候变化与人为干扰背景下,川金丝猴生境格局时空变化特征,为野生濒危动物生境保护管理和政策制定提供科学依据。     

华北平原玉米叶片光合及呼吸过程对实验增温的适应性

利用典型农田生态系统的原位实验增温平台,探讨我国华北平原重要农作物玉米叶片光合及呼吸过程对实验增温的适应性,并深入分析其产生适应性的原因和机理。研究结果显示,实验增温使玉米叶片净光合速率(A_n)显著升高(P0.001),同时增温也导致A_n的最适温度(T_(opt))升高1.56℃;相似地,实验增温也同样导致了光合作用过程中最大电子传递速率(J_(max))显著增加(P0.001),并且其最适温度(T_(opt))升高了1.45℃,但并没有对最大羧化反应速率(V_(cmax))及其温度敏感性(Q_(10))产生显著的影响(P0.05)。然而,实验增温却显著降低了玉米叶片的暗呼吸速率(R_d)及其Q_(10)值(P0.05)。另外,研究结果还显示实验增温没有对R_d/A_g和J_(max)/V_(cmax)产生显著的影响(P0.05)。此外,尽管实验增温显著提高了玉米叶片的蒸腾速率(T_r),但却并没有显著改变叶片的气孔导度(G_s)及水分利用效率(WUE)。研究结果表明,玉米可以通过调控叶片光合及呼吸等关键生理过程的最适温度对增温产生一定的适应性。然而,尽管玉米能够在叶片尺度上做出调整来适应增温环境,但这种适应能力却十分有限,以至于未来气候变暖仍可能会对华北平原玉米的生长发育过程和粮食产量造成一定的影响。     

气候变化对黑龙江省水稻障碍型冷害的影响

明确气候变化对黑龙江省水稻孕穗期和抽穗期障碍型冷害的影响,可为水稻安全生产提供科学依据。基于黑龙江省70个台站1971—2012年的气象资料和10个台站1980—2011年水稻生育期数据,结合水稻障碍型冷害指标,分析了气候变化对黑龙江省水稻障碍型冷害的影响。结果表明:(1)水稻孕穗期障碍型冷害1990s发生频率最低,2000s发生频率最高;抽穗期障碍型冷害1970s和1980s发生频率高,1990s和2000s发生频率低。(2)抽穗期障碍型冷害发生程度大于孕穗期障碍型冷害。(3)不同熟型水稻品种可种植北界逐渐北移东扩,极早熟、早熟和中熟品种可种植范围分别缩小了5、21和11个县(市),中晚熟和晚熟品种可种植范围分别扩大了14和23个县(市)。(4)随着水稻种植格局的变化,不同熟型水稻障碍型冷害均在1990s发生频率最低,2000s发生频率最高。     

A genetically distinct hybrid zone occurs for two globally invasive mosquito fish species with striking phenotypic resemblance

Hybrid zones allow for the investigation of incipient speciation and related evolutionary processes of selection, gene flow, and migration. Interspecific dynamics, like competition, can impact the size, shape, and directional movement of species in hybrid zones. Hybrid zones contribute to a paradox for the biological species concept because interbreeding between species occurs while parental forms remain distinct. A long‐standing zone of intergradation or introgression exists for eastern and western mosquito fish (Gambusia holbrooki and G. affinis) around Mobile Bay, AL. The region has been studied episodically, over decades, making it perfect for addressing temporal dynamics and for providing a deeper understanding of the genetics of these periodically reclassified fishes (as species or subspecies). We used six microsatellite markers to assess the current population structure and gene flow patterns across 19 populations of mosquito fish and then compared our results with historical data. Genetic evidence demonstrates that the current hybrid zone is located in a similar geographic region as the historical one, even after three decades. Hybrid fish, however, demonstrate relatively low heterozygosity and are genetically distinct from western and eastern mosquito fish populations. Fin ray counts, sometimes used to distinguish the two species from one another, demonstrate more eastern (G. holbrooki) phenotype fish within the molecular genetic hybrid zone today. Mosquito fish are globally invasive, often found on the leading edge of flooded waters that they colonize, so the impact of hurricanes in the wake of climate change was also evaluated. An increase in the frequency and intensity of hurricanes in the hybrid region has occurred, and this point warrants further attention since hurricanes are known to move these aggressive, invasive species into novel territory. This work contributes to our classical understanding of hybrid zone temporal dynamics, refines our understanding of mosquito fish genetics in their native range, evaluates important genotype–phenotype relationships, and identifies a potential new impact of climate change.     

Species selection and random drift in macroevolution

Species selection resulting from trait‐dependent speciation and extinction is increasingly recognized as an important mechanism of phenotypic macroevolution. However, the recent bloom in statistical methods quantifying this process faces a scarcity of dynamical theory for their interpretation, notably regarding the relative contributions of deterministic versus stochastic evolutionary forces. I use simple diffusion approximations of birth‐death processes to investigate how the expected and random components of macroevolutionary change depend on phenotype‐dependent speciation and extinction rates, as can be estimated empirically. I show that the species selection coefficient for a binary trait, and selection differential for a quantitative trait, depend not only on differences in net diversification rates (speciation minus extinction), but also on differences in species turnover rates (speciation plus extinction), especially in small clades. The randomness in speciation and extinction events also produces a species‐level equivalent to random genetic drift, which is stronger for higher turnover rates. I then show how microevolutionary processes including mutation, organismic selection, and random genetic drift cause state transitions at the species level, allowing comparison of evolutionary forces across levels. A key parameter that would be needed to apply this theory is the distribution and rate of origination of new optimum phenotypes along a phylogeny.