Using primary productivity as an index of coastal eutrophication: the units of measurement matter

Eutrophication is a serious environmental and economic problemin coastal marine ecosystems worldwide. It has recently beenrecommended that measurements of primary productivity, beinga sensitive and accurate indicator of eutrophication, shouldbe mandatory when monitoring and assessing the ecological statusof coastal waters. The units of primary productivity chosenfor eutrophication assessment will be very important becausenot all measures of primary productivity vary monotonically(or even straightforwardly) with changes in aquatic fertility.Volumetric expressions of primary productivity (rates of carbonfixation per unit volume of seawater) may prove to be the mostsensitive and most reliable measures to use when evaluatingthe eutrophication status of coastal marine ecosystems. Anotherpotential measure of primary productivity, the light-saturatedrate of photosynthesis per unit Chlorophyll a (P:B^Chl) ratio,is unsuitable for the assessment of aquatic ecosystem responsesto nutrient enrichment.     

Limitations on photosynthesis of competing individuals in stands and the consequences for canopy structure

The canopy structure of a stand of vegetation is determined by the growth patterns of the individual plants within the stand and the competitive interactions among them. We analyzed the carbon gain of individuals in two dense monospecific stands of Xanthium canadense and evaluated the consequences for intra-specific competition and whole-stand canopy structure. The stands differed in productivity, and this was associated with differences in nitrogen availability. Canopy structure, aboveground mass, and nitrogen contents per unit leaf area (N_area) were determined for individuals, and leaf photosynthesis was measured as a function of N_area. These data were used to calculate the daily carbon gain of individuals. Within stands, photosynthesis per unit aboveground mass (P_mass) of individual plants increased with plant height, despite the lower leaf area ratios of taller plants. The differences in P_mass between the tallest most dominant and shortest most subordinate plants were greater in the high-nitrogen than in the low-nitrogen stand. This indicated that competition was asymmetric and that this asymmetry increased with nitrogen availability. In the high-nitrogen stand, taller plants had a higher P_mass than shorter ones, because they captured more light per unit mass and because they had higher photosynthesis per unit of absorbed light. Conversely, in the low-nitrogen stand, the differences in P_mass between plants of different heights resulted only from differences in their light capture per unit mass. Sensitivity analyses revealed that an increase in N_area, keeping leaf area of plants constant, increased whole-plant carbon gain for the taller more dominant plants but reduced carbon gain in the shorter more subordinate ones, which implies that the N_area values of shorter plants were greater than the optimal values for maximum photosynthesis. On the other hand, the carbon gain of all individual plants, keeping their total canopy N constant, was positively related to an increase in their individual leaf area. At the same time, however, increasing the leaf area for all plants simultaneously reduced the carbon gain of the whole stand. This result shows that the optimal leaf area index (LAI), which maximizes photosynthesis of a stand, is not evolutionarily stable because at this LAI, any individual can increase its carbon gain by increasing its leaf area.     

基于全球净初级生产力的能源足迹计算方法

净初级生产力是当前生态足迹改进研究的重要突破口。针对传统能源足迹存在着忽略多数土地的碳吸收贡献、碳吸收能力界定不清等不足,提出了基于全球平均净初级生产力的能源足迹计算方法。结果表明:单位质量能源的生态足迹空间构成中,前3位依次为海洋、林地和草地,分别占28.32%、27.25%、21.77%。单位空间占用面积的能源热值由高至低依次为电力、气态、液态和固态能源,分别达2.11×106—9.76×107、108—116、88—99、68—72 GJ/hm2。对各类能源生态影响的判断均较传统方法乐观,这是综合考虑全球各类土地和水体碳吸收贡献的结果。基于全球净初级生产力的能源足迹反映了能源消费的空间占用平均水平,有助于提高评价结果的真实性与准确性。     

北京山区3种暖温带森林生态系统未来碳平衡的模拟与分析

使用LPJ-GUESS植被动态模型, 在北京山区研究了未来100a以辽东栎 (Quercus liaotungensis) 为优势种的落叶阔叶林、以白桦 (Betula platyphylla) 为主的阔叶林和油松 (Pinus tabulaeformis) 为优势种的针阔混交林的碳变化, 定量分析了生态系统净初级生产力 (NPP) 、土壤异养呼吸 (Rh) 、净生态系统碳交换 (NEE) 和碳生物量 (Carbon bio-mass) 对两种未来气候情景 (SRES A2和B2) 以及相应大气CO2浓度变化情景的响应特征。结果表明:1) 未来100a两种气候情景下3种森林生态系统的NPP和Rh均增加, 并且A2情景下增加的程度更大;2) 由于3种生态系统树种组成的不同, 未来气候情景下各自NPP和Rh增加的比例不同, 导致三者NEE的变化也相异:100a后辽东栎林由碳汇转变为弱碳源, 白桦林仍保持为碳汇但功能减弱, 油松林成为一个更大的碳汇;3) 3种森林生态系统的碳生物量在未来气候情景下均增大, 21世纪末与20世纪末相比:辽东栎林在A2情景下碳生物量增加的比例为27.6%, 大于B2情景下的19.3%;白桦林和油松林在B2情景下碳生物量增加的比例分别为34.2%和52.2%, 大于A2情景下的30.8%和28.4%。     

The Supply of Air to Leaves in Assimilation Chambers

Factors affecting the supply of air to leaves enclosed in assimilationchambers have been studied using models and leaves of appleand plum. The rate of CO₂ assimilation of a leaf does not increaselinearly with increasing rate of air flow. Explanations of thisand other observations are put forward in terms of the boundary-layerconcept and diffusion paths. Comparisons are made with free-airconditions, and it is concluded that air should be suppliedat the same rate (ml/min) for leaves of different size in thesame chamber. Three cup designs were also studied. A methodis described for making valid comparisons of assimilation ratesper unit area by extrapolation to an infinitely high rate ofair flow. Measurements of different sized leaves with chambersand cups can be compared in this way. Rates expressed per unitarea can be correctly compared only if the resistance to diffusionoutside the leaf is negligible, or under special conditions.Assimilation rates measured with rates of air flow giving CO₂availability equivalent to that occurring in static free airshould be expressed per unit perimeter. Methods of correctionof assimilation rates for the depletion of carbon dioxide fromthe air stream are considered.     

Studies on Biodiversity in the Plankton, Benthos, and Fish Communities, and the Ecosystems of Fresh Water Bodies Differing in Productivity

The species diversity of phyto- and zooplankton, benthic animals, and ichthyofauna was studied in continental water bodies that differ in type, geographic location, size, and productivity. The results showed that the number of species in the communities of aquatic organisms and in ecosystems depends on the area and volume of the water body and the level of plankton primary production. Corresponding relationships can be approximated by the equations of exponential and polymodal functions. The species number and biomass per unit area or volume proved to decrease as the area or volume of the water body increased. The greatest number of heterotrophic species was observed in water bodies whose primary production approached 1400 kcal/m² per year. It is proposed that the number of aquatic species in a body of water depends on the total area of the latter and the area of individual territories occupied by the representatives of certain species.     

Nitrogen Productivity Depends on Photosynthetic Nitrogen Use Efficiency and on Nitrogen Allocation Within the Plant

The concept of plant nitrogen productivity was introduced atthe end of the 1970s to interpret the dependency of plant growthon internal nitrogen. It is defined as the increase in plantdry matter per unit time and per unit plant nitrogen content.Recently, plant nitrogen productivity has been expressed asthe product of two terms: the leaf nitrogen ratio, which isthe proportion of the plant's nitrogen present in the leaves,and the leaf nitrogen productivity, which is defined as theincrease in plant dry matter per unit time and leaf nitrogencontent. In the present paper we use two data sets obtainedfrom C₃ herbaceous species to evaluate the relative importanceof variation in leaf nitrogen ratio and leaf nitrogen productivityin determining interspecific variation in plant nitrogen productivity.Further, we analyse to what extent leaf and plant nitrogen productivitiesdepend on photosynthetic nitrogen use efficiency. Results showthat in all cases, photosynthetic nitrogen use efficiency isa major determinant of both plant and leaf nitrogen productivities.A positive relationship between leaf nitrogen ratio and plantnitrogen productivity was found only when comparisons were madeover broad taxonomic groups.Copyright 1995, 1999 Academic Press Interspecific variation, leaf nitrogen ratio, nitrogen productivity, photosynthetic nitrogen use efficiency     

庐山风景区碳源、碳汇的测度及均衡

旅游目的地系统碳源、碳汇的计算与分析,不仅是旅游业节能减排政策制定的重要依据,也是旅游与环境相互关系研究的一个新的科学命题.以庐山风景区为例,计算并分析了2010年的碳源及碳汇.结果表明:(1)2010年庐山风景区包括本地居民和旅游者的总碳排放为108 697 t.其中,本地居民占碳排放总量的19.52％,旅游者占碳排放总量的80.48％.在旅游者碳排放中,旅游交通碳排放占50.24％,旅游住宿碳排放占38.04％,旅游食物消费碳排放占10.65％,旅游活动碳排放仅占1.07％;(2)2010年庐山风景区内陆地生态系统碳吸收为9447 t;(3)从碳源、碳汇均衡角度看,庐山陆地生态系统的固碳量吸收了区内碳排放的23.47％.但由于旅游者的区际流动和旅游业的产业关联性强,陆地生态系统的碳吸收仅占区内和区外碳排放总量的8.69％,旅游业使庐山成为一个显著的碳源.     

Frequency of Dividing Cells, a New Approach to the Determination of Bacterial Growth Rates in Aquatic Environments

Frequency of dividing cells is suggested to be an indirect measure of the mean growth rate of an aquatic bacterial community. Seasonal changes in frequency of dividing cells were found which covariated with the bacterial uptake of ¹⁴C-labeled phytoplankton exudates. Batch and continuous culture growth experiments, using brackish water bacteria in pure and mixed enrichment cultures, were performed to establish a relationship between frequency of dividing cells and growth rate. An improved technique for bacterial direct counts, using fluorescent staining and epifluorescence microscopy, is presented. Based on a 6-month survey in a coastal area of the Baltic Sea, the bacterial production in the photic zone is estimated. Compared to the total primary production in the area, the bacterial population during this period utilized approximately 25% of the amount of carbon originally fixed by the primary producers.     

Water Stress, CO2 and Climate Change

Climatic change may bring about increased aridity to large areasof Europe. Higher temperatures, larger water deficits and highlight stress are likely to occur in conjunction with elevatedatmospheric CO₂. This raises the question whether a high CO₂concentration in the atmosphere can compensate for the decreasein carbon gain in water-stressed plants. The processes whichdetermine dry matter production and the ways they are affectedby soil water deficits are discussed. It is now well establishedthat in most species and under most circumstances stomata arethe main limiting factor to carbon uptake under water deficit,the photosynthetic machinery being highly resistant to dehydration.However, when other stresses are superimposed, a decline inphotosynthetic capacity may be observed. In the short term,under drought conditions, the increase in CO₂ in the atmospheremay diminish the importance of stomatal limitation for carbonassimilation, inhibit photorespiration, stimulate carbon partitioningto soluble sugars and increase water-use efficiency. Some recentevidence seems to indicate that under conditions of high irradiance,plants growing at elevated CO₂ may develop protection towardsphotoinhibition, which might otherwise result in significantlosses in plant production under stress conditions. In the longerterm though, a negative acclimation of photosynthesis appearsto occur in many species, an explanation for which still needsto be clearly identified. Similarly, the effects of extendedexposure to elevated CO₂ under arid conditions are not known.Plant production is more closely related to the integral ofphotosynthesis over time and total foliage area than to theinstantaneous rates of the photosynthetic process. Water deficitsresult in a decrease in foliage area biomass and, therefore,in productivity. On the other hand, the increase in air temperaturemay result in more respiratory losses. However, experimentalas well as simulatory evidence suggests that doubling CO₂ concentrationin the air may improve carbon assimilation and compensate partiallyfor the negative effects of water stress even if we assume adown-regulation of the photosynthetic process as a result ofacclimation to elevated CO₂.     

遮阴对黄波罗幼苗的光合特性及光能利用效率的影响

一直以来黄波罗(Phellodendron amurense)被认为是不耐阴树种, 然而引入美国纽约后, 发现它具有一定的耐阴性, 在全光和林下均能更新, 在纽约已经成为生物入侵种。为了探讨黄波罗的耐阴性问题, 通过设置自然光与遮阴(15%自然光)两种光环境, 观测了三年生黄波罗幼苗(遮阴1 a后)光合生理参数、光能利用效率、叶绿素和比叶重的变化。结果表明, 与自然光处理相比, 遮阴处理的黄波罗幼苗最大光合速率、表观量子效率和暗呼吸速率略有下降, 但差异不显著(p>0.05), 光补偿点下降显著(p＜0.05); 同时, 单位面积叶绿素含量无显著差异(p>0.05), 而单位干重叶绿素含量显著升高, 比叶重显著下降, 叶面积显著增大(p＜0.05)。上述结果说明: 遮阴的黄波罗幼苗通过降低光补偿点和暗呼吸速率利用环境中的弱光, 同时通过减小比叶重、增大叶面积和提高叶绿素b相对含量来增强对光的捕获, 使其在弱光时的光能利用效率提高。由此推断, 黄波罗幼苗能适应一定程度的遮阴。     

Chlorophyll a fluorescence in phytoplankton: relationship to photosynthesis and biomass

The theoretical and applied aspects of in vivo chlorophyll fluorescenceare reviewed for aquatic biologists who use fluorescence inestimating standing stocks and photosynthetic activity. Themajor advantage of using fluorescence is that the measurementis easy to make. However, despite some sound theoretical modelsdescribing variable fluorescence there are many environmentalfactors influencing fluorescence about which little is known.Much more basic research on fluorescence-photosynthesis relationshipsneeds to be done before fluorescence per se can replace current¹⁴C or O₂ methods for measuring primary productivity. ^*This paper is the result of a study made at the Group for AquaticPrimary Productivity (GAP), Second International Workshop heldat the National Oceanographic Institute, Haifa, Israel in April–May1984.     

Spatial and temporal photosynthetic compartments during summer in Antarctic Lake Kitiesh

Summary Four autotrophic compartments were recognised in Lake Kitiesh, King George Island (Southern Shetland) at the beginning of the summer in 1987: snow microalgae, ice bubble communities, phytoplankton in the water column and benthic communities of moss with epiphytes. Chlorophyll a concentration and pigment absorption spectra were obtained in these four compartments before and/or after the thawing of the ice cover. During the ice free period, carbon fixation and biomass was measured in the phytoplankton and in the benthic moss Campyliadelphus polygamus. From these measurements we conclude that the benthic moss is the most significant autotrophic component in this lake in terms of biomass, chlorophyll a content and primary productivity. The integral assimilation number (The ratio of carbon fixation per unit area to biomass per unit area) values were similar for both phytoplankton and the moss, ranging from 3.6 to 5.4 mg C (mg Chl a)^–1h^–1in phytoplankton and from 4.0 to 6.4 mgC (mg Chl a)^–1h^–1 in the benthic moss. This approach allows comparisons of carbon fixation efficiency of the chlorophyll a under a unit area between compartments in their different light environments.     

Models of the Use of Root-zone CO2 by Selected North American Isoetids

Sediment CO₂, entering via the roots, contributes a significantportion of the total carbon uptake for isoetids (small, evergreen,submersed, vascular plants). Laboratory studies of inorganiccarbon uptake via the roots and shoots by five isoetids wereused to model the use of root-zone CO₂. Simple first-order linearmodels accounted for at least 75 per cent of the variation inthe data for Gratiola aurea, Isoetes macrospora, Littorellauniflora and Lobelia dortmanna. For Eriocaulon septangulare,which relies almost exclusively on root-zone CO₂, models couldaccount for only about 62 per cent of the variation in root-zoneCO₂ use. For each species, we present the best fitting regressionof root-zone CO₂ use as a function of root- and shoot-zone CO₂concentrations. For the species studied, carbon uptake was not saturated atfield concentrations of root and shoot-zone CO₂. Maximum ratesof carbon uptake were lower for species that naturally occurredat greater depths, compared with species more common in shallowwater. At equal external CO₂ concentrations carbon entry perunit root surface area was several times more rapid than entryper unit shoot surface area for L. dortmanna. The entry ratesper unit root and shoot surface area were about equal for G.aurea and E. septangulare. Shoots were equally or more permeablethan the roots of L. uniflora and I. macrospora, a fact thatmay be related to the functioning of crassulacean acid metabolismin these plants. Carbon, CO₂, photosynthesis, isoetid, Eriocaulon septangulare, Gratiola aurea, Isoetes macrospora, Littorella uniflora, Lobelia dortmanna     

Temperate Grassland Responses to Climate Change: an Analysis using the Hurley Pasture Model

The Hurley Pasture Model is process-based and couples the carbon,nitrogen and water cycles in the soil-grass-animal system. Itwas used to examine the responses of grasslands in southern,lowland and northern, upland climates in Britain. Short-termresponse to step-wise increases in CO₂concentration (350 to700 µmol mol^-1) and temperature (5 °C) were contrastedwith long-term equilibrium (the term ‘equilibrium’is equivalent to ‘steady state’ throughout thispaper) responses and with responses to gradually increasing[CO₂] and temperature. Equilibrium responses to a range of climatevariables were also examined. Three conclusions were drawn regarding the interpretation ofexperiments: (1) initial ecosystem responses to step-wise changescan be different in both magnitude and sign to equilibrium responses,and this can continue for many years; (2) grazing can drasticallyalter the magnitude and sign of the response of grasslands toclimate change, especially rising temperatures; and (3) effectsof changes in climate, especially temperature and rainfall,are likely to be highly site-specific. It was concluded thatexperiments should try to lessen uncertainty about processeswithin models rather than try to predict ecosystem responsesdirectly. Three conclusions were also drawn about the operation of grasslandsas carbon sinks: (1) increasing [CO₂] alone will produce a carbonsink, as long as it continues to accelerate photosynthesis andincrease net primary productivity; (2) by contrast, increasingtemperatures alone are likely to produce a carbon source, becausesoil respiration is accelerated more than net primary productivity,even when assuming the same temperature function for most soiland plant biochemical processes; and (3) the net effect of projectedincreases in [CO₂] and temperature is likely to be a carbonsink of 5–15 g C m^-2yr^-1in humid, temperate grasslandsfor several decades, which is consistent with the magnitudeof the hypothesized current global terrestrial carbon sink. Grassland; climate change; carbon dioxide; temperature; ecosystem; model; carbon sink     

Effect of Water Stress on Photosynthesis, Leaf Characteristics and Productivity of Field-Grown Nicotiana tabacum L. Genotypes Selected for Survival at Low CO2

Dry mass production, leaf characteristics and diurnal photosynthesisof two N. tabacum L. genotypes selected for survival at lowCO₂ and the parent Wisconsin-38 (control plants) were measuredon water-stressed and well-watered plants in the field. Differencesin photosynthesis per unit leaf area were small and not significantbetween genotypes, but different patterns of photosynthesiswere observed in stressed and non-stressed plants, with waterstress reducing total net carbon fixation by 45% in all genotypes.More dry mass was produced by the selected genotypes than byWisconsin-38 under irrigation. Production was smaller and thesame for all three genotypes when stressed. The increased drymass of the selected genotypes was related to greater totalleaf area per plant which was accompanied by more cells perunit leaf area but smaller cell volume than in the control plants.The decrease in dry mass production under water stress was relatedto a decrease in total leaf area per plant and a decrease incell number per unit leaf area; however, cell volume increased. Key words: Water stress, photosynthesis, productivity, leaf cells, genotype     

中亚热带人工针叶林对未来气候变化的响应

利用基于生理生态学过程的EALCO模型,探讨了千烟洲中亚热带人工针叶林生态系统对未来气候变化的响应.结果表明:CO₂浓度、温度和降水的变化对该人工林生态系统碳水通量影响的程度不同,其中CO₂浓度＞温度＞降水.CO₂浓度是生态系统总光合生产力(GPP)的主要驱动因子,温度与CO₂浓度均是控制生态系统呼吸的主要环境因子,温度的升高使植物地上部分呼吸明显增加,而CO₂浓度升高则对土壤呼吸影响较大.温度升高使蒸散(ET)增加,而CO₂浓度升高则使ET减少.在未来气候变化情景(2100年)下,该人工林生态系统的净初级生产力将增加22%,说明其仍具有较强的固碳潜力.     

气候变暖对陆地生态系统碳循环的影响

作为全球变化的主要表现之一,气候变暖对全球陆地生态系统碳循环的影响巨大,揭示这一作用对于精确理解碳循环的过程和相关政策的制定具有重要的指导意义。该文综述了此领域近十几年来的主要研究工作,总结了陆地生态系统碳循环对气候变暖响应的主要内部机制及其过程,简述了相关模型的发展及其主要应用,并指出以往研究中存在的主要问题以及未来研究的主要方向。在气候变暖条件下,陆地生态系统碳循环的变化主要体现在以下几个方面:1)低纬度地区生态系统NPP一般表现为降低,而在中高纬度地区通常表现为增加,而在全球尺度上表现为NPP增加;2)土壤呼吸作用增强,但经过一段时间后表现出一定的适应性;3)高纬度地区的生态系统植被碳库表现为增加趋势,低纬度地区生态系统植被碳库变化不大,或略微降低,在全球尺度上表现为植被碳库增加;4)地表凋落物的产量和分解速率增加;5)土壤有机碳分解加速,进而减少土壤碳储存,同时植被碳库向土壤碳库的流动增加从而增加土壤碳库,这两种作用在不同生态系统的比重不同,在全球尺度上表现为土壤碳库的减少;6)尽管不同生态系统表现各异,总体上全球陆地生态系统表现为一个弱碳源。生物物理模型、生物地理模型和生物地球化学模型陆续被开发出来用于研究工作,并取得了一定的成果,但是研究结果仍然存在很大的不确定性。在未来的数年甚至是数十年间,气候变暖与全球变化的其它表现间的协同影响将是下一步的研究重点,气候变暖和陆地生态系统间的双向反馈作用机制是进行更准确研究的理论基础,生态系统结构和功能对气候变化的适应性是准确理解和预测未来气候情景下陆地生态系统碳循环的前提。     

不同碱度条件下中华水韭昼夜CO2气体交换的特征

 运用pH-drift的方法研究了在不同碱度条件下中华水韭(Isoetes sinensis)的沉水叶片昼夜CO₂吸收的特征。结果表明中华水韭的沉水叶片具有昼夜吸收水中CO₂的能力, 而不具备利用水中的HCO ₃^–的能力, 进一步证明了水生植物中华水韭的光合碳同化途径具有景天酸代谢(CAM)的特征。中华水韭沉水叶片光照条件下对水中CO₂的吸收速率在一定的浓度范围内正相关于水中的CO₂浓度。光照条件下, 中华水韭的pH-drift实验的pH补偿点分别为(8.1±0.3)和(7.9±0.1) mmol·L^–1, 最终[CT]/Alk值为(1.009±0.01)和(1.022±0.004)。碱度对中华水韭夜晚CO2的吸收速率有显著的影响(F = 38.73, p < 0.000 1)。总碱度1.70 mmol·L^–1溶液中的中华水韭沉水叶片在相对较低的CO₂浓度(0.04±0.001 mmol·L^–1)水平下即表现出对CO₂的净吸收。调查了野外一处中华水韭沉水种群的生境pH值及CO₂浓度的昼夜变化, 发现水体碱度约为1.59 mmol·L^–1, 一昼夜的pH值波动不大, 平均为(6.1±0.04), 昼夜CO₂浓度存在波动, 午夜水中的CO₂浓度是午后的近3倍。     

Aquatic carbon fluxes dampen the overall variation of net ecosystem productivity in the Amazon basin: An analysis of the interannual variability in the boundless carbon cycle

The river–floodplain network plays an important role in the carbon (C) cycle of the Amazon basin, as it transports and processes a significant fraction of the C fixed by terrestrial vegetation, most of which evades as CO₂ from rivers and floodplains back to the atmosphere. There is empirical evidence that exceptionally dry or wet years have an impact on the net C balance in the Amazon. While seasonal and interannual variations in hydrology have a direct impact on the amounts of C transferred through the river–floodplain system, it is not known how far the variation of these fluxes affects the overall Amazon C balance. Here, we introduce a new wetland forcing file for the ORCHILEAK model, which improves the representation of floodplain dynamics and allows us to closely reproduce data‐driven estimates of net C exports through the river–floodplain network. Based on this new wetland forcing and two climate forcing datasets, we show that across the Amazon, the percentage of net primary productivity lost to the river–floodplain system is highly variable at the interannual timescale, and wet years fuel aquatic CO₂ evasion. However, at the same time overall net ecosystem productivity (NEP) and C sequestration are highest during wet years, partly due to reduced decomposition rates in water‐logged floodplain soils. It is years with the lowest discharge and floodplain inundation, often associated with El Nino events, that have the lowest NEP and the highest total (terrestrial plus aquatic) CO₂ emissions back to atmosphere. Furthermore, we find that aquatic C fluxes display greater variation than terrestrial C fluxes, and that this variation significantly dampens the interannual variability in NEP of the Amazon basin. These results call for a more integrative view of the C fluxes through the vegetation‐soil‐river‐floodplain continuum, which directly places aquatic C fluxes into the overall C budget of the Amazon basin.