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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Endangered ecosystems. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (470 pages)
    Edition: 1st ed.
    ISBN: 9783662499023
    Series Statement: Ecological Studies ; v.227
    DDC: 551.51098616
    Language: English
    Note: Intro -- Preface -- Contents -- Part I: Introduction -- Chapter 1: Interactions Between Biosphere, Atmosphere, and Human Land Use in the Amazon Basin: An Introduction -- 1.1 The Amazon Basin -- 1.2 The LBA Projects 1998-2007 -- 1.3 This Book -- References -- Part II: Biosphere-Atmosphere Interactions -- Chapter 2: Biogenic Volatile Organic Compounds in Amazonian Forest Ecosystems -- 2.1 Introduction -- 2.2 BVOC Biosynthesis in Plants -- 2.3 Volatile Metabolomics -- 2.4 BVOCs as Biomarkers of Lipid Peroxidation Under Oxidative Stress -- 2.5 BVOC Bidirectional Biosphere-Atmosphere Exchange -- 2.6 Conclusions -- References -- Chapter 3: The Hydrology and Energy Balance of the Amazon Basin -- 3.1 Introduction -- 3.2 Current Conditions -- 3.2.1 Mean Conditions and Spatial Variability -- 3.2.2 Temporal Variability -- 3.3 Anthropogenic Influences -- 3.3.1 Land Cover and Land Use Change -- 3.3.1.1 Vegetation Controls on Water/Energy Balance -- 3.3.1.2 Land Use Impacts on the Water/Energy Balance -- 3.3.2 Global Climate Change -- 3.4 Conclusions -- References -- Chapter 4: Extreme Seasonal Climate Variations in the Amazon Basin: Droughts and Floods -- 4.1 Introduction -- 4.2 History of Hydro-meteorological Extremes in the Region: Inter-annual Variability of Rainfall/Rivers in the Basin -- 4.3 Long-Term Variability and Trends of Hydro-meteorological Extremes -- 4.4 Projected Climate Change in Amazonia -- 4.5 Regional Extremes and Impacts on Future Climate Change Scenarios -- 4.6 Conclusions -- References -- Part III: Carbon Balance -- Chapter 5: The Amazon Carbon Balance: An Evaluation of Methods and Results -- 5.1 Introduction -- 5.2 Evaluation of Methods -- 5.2.1 Bottom-Up Estimates -- 5.2.1.1 Biomass Plots -- 5.2.1.2 Eddy Covariance Sites -- 5.2.2 Top-Down Estimates -- 5.2.2.1 Measurements from Air-Borne Platforms. , 5.2.2.2 Measurements from the Global Atmospheric Network -- 5.2.3 The Role of Satellite Remote Sensing -- 5.3 Evaluation of Results, with Emphasis on Uncertainties Arising from Methods -- 5.3.1 What Is the Carbon Balance of the Amazon Basin? -- 5.3.1.1 FDeforestation and FDegradation the Deforestation and Degradation Fluxes -- 5.3.1.2 Fold-growth and FSecondary Fluxes Over Forests -- 5.3.1.3 FPlantation -- 5.3.1.4 FHarvest -- 5.3.1.5 FPeat -- 5.3.1.6 FAgriculture -- 5.3.1.7 FClimatechange -- 5.3.1.8 FFossilfuel -- 5.3.2 Total Estimate of Carbon Balance, Bottom-Up Evaluation -- 5.3.3 Total Estimate of Carbon Balance, Top-Down Evaluation -- 5.4 Answers to the Science Questions -- 5.4.1 What Is the Carbon Balance of the Amazon, and How Does It Change from Year to Year According to Climatological Variation... -- 5.4.2 What Is the Seasonality in the Carbon Flux Between the Land and Atmosphere? -- 5.4.3 How Do the Changes in Land Use Affect the Fluxes? -- References -- Chapter 6: Climate and the Amazonian Carbon Balance -- 6.1 Introduction -- 6.2 Climate Background -- 6.3 Flux Components of the Amazon Carbon Balance -- 6.3.1 Carbon Release Caused by Deforestation -- 6.3.2 Intact Forest Carbon Balance -- 6.3.3 Fossil Fuel Emissions -- 6.3.4 Riverine Carbon -- 6.3.5 Amazon-Wide Carbon Balance Based on Lower Troposphere Greenhouse Gas Balances -- 6.4 Summary and Conclusions -- Appendix: Formalisation of Book Keeping Approach to Estimate Carbon Fluxes Caused by Deforestation Based on Data of Area Defor... -- Carbon Release to the Atmosphere After Deforestation -- Carbon Uptake from the Atmosphere by Re-establishing land Vegetation -- References -- Chapter 7: Aquatic Ecosystems -- 7.1 Introduction -- 7.2 Inundation and the Variable Extent of Aquatic Habitats: Remote Sensing and Modelling -- 7.2.1 Remote Sensing. , 7.2.2 Geomorphological Approaches to River Areas -- 7.2.3 Modelling of Inundation -- 7.3 Gas Transfer Velocity Between Water and Atmosphere -- 7.4 Carbon Dioxide and Methane Concentrations and Fluxes -- 7.4.1 Streams and Rivers -- 7.4.2 Lakes -- 7.4.3 Wetlands -- 7.4.4 Reservoirs -- 7.4.5 Airborne Surveys -- 7.5 Regionalisation of Fluxes -- 7.5.1 Prior Estimates -- 7.5.2 New Estimates -- 7.6 Sources and Decomposition of Organic Carbon -- 7.7 Uncertainties and Research Needs -- 7.7.1 Field Measurements -- 7.7.2 Modelling -- 7.8 Climate Change, Exceptional Events, and Human Impacts -- 7.9 Conclusion -- References -- Chapter 8: Ecosystem-Atmosphere Exchanges of CO2 in Dense and Open `Terra Firme´ Rainforests in Brazilian Amazonia -- 8.1 Introduction -- 8.2 Sites: Rainfall Patterns and Precipitation Seasonality -- 8.3 Ecosystem-Atmosphere CO2 Fluxes in BLA -- 8.4 Seasonality of C-Fluxes -- 8.5 Seasonality of Photosynthesis -- 8.6 Inter-annual Variability -- 8.7 Conclusions -- References -- Chapter 9: Overview of Forest Carbon Stocks Study in Amazonas State, Brazil -- 9.1 Background -- Box 9.1: Reducing Emissions from Deforestation and Forest Degradation (REDD-plus) -- 9.2 Development of Allometric Equations -- 9.2.1 Allometric Equations for Old-Growth Amazonian Forests -- Box 9.2: Data Collection for Developing Allometric Models -- Box 9.3: Uncertainty -- 9.2.2 Common Allometry with Dominant Height -- 9.3 Plot-Based Carbon Stock Estimation -- 9.3.1 Structural Features of Inventory Plots -- Box 9.4: Forest Inventory -- Box 9.5: Description of the Sites Where Biomass Destructive Allometry Were Conducted -- 9.3.2 Carbon Stock Estimation -- 9.4 Perspective for Future Studies on the Carbon Stocks in Amazonas State -- References -- Part IV: Environmental Variation and Global Change -- Chapter 10: Recent Changes in Amazon Forest Biomass and Dynamics. , 10.1 Introduction -- 10.1.1 Overview -- 10.1.2 A Networked Approach -- 10.2 Methods -- 10.3 Results and Discussion -- 10.3.1 Structural Change -- 10.3.2 Recovery from Large Disturbances? -- 10.3.3 Dynamic Changes -- 10.3.4 Functional Compositional Changes -- 10.3.5 Recent Drought Impacts in Amazonia -- 10.3.6 What is Driving these Changes? -- 10.3.7 The Future: Potential Susceptibility of Amazon Forest to Environmental Stress and Compositional Changes -- 10.3.7.1 Moisture Stress -- 10.3.7.2 Photosynthesis/Respiration Changes -- 10.3.7.3 Compositional Change -- 10.4 Conclusion -- References -- Chapter 11: The Biogeochemistry of the Main Forest Vegetation Types in Amazonia -- 11.1 Introduction -- 11.2 Physiography and the Atmosphere-Vegetation-Soil System in the Major Vegetation Formations of the Amazon Basin -- 11.2.1 Introduction: Nutrient Cycles -- 11.2.2 Physiography of the Amazon Basin -- 11.3 Carbon -- 11.3.1 Carbon Stocks, Allocation, and Fluxes -- 11.3.1.1 Carbon Stocks -- 11.3.1.2 Carbon Fluxes -- 11.4 Nitrogen and Phosphorus -- 11.4.1 External Sources -- 11.4.1.1 Nitrogen Fixation -- 11.4.1.2 Atmospheric Deposition and Canopy Leaching -- 11.4.2 Nitrogen and Phosphorus Stocks and Fluxes -- 11.4.2.1 Stocks -- 11.4.2.2 Fluxes -- 11.4.3 Losses -- 11.4.3.1 Leaching, Surface and Subterranean Flows, and Stream Export of N, P, and C -- 11.4.3.2 N Trace Gas Emissions -- 11.4.3.3 Biogenic Volatile Organic Compounds -- 11.5 Synthesis and Conclusions -- 11.5.1 Emerging Patterns for Elemental Cycles Across Forest Formations -- 11.5.1.1 Carbon -- 11.5.1.2 Nitrogen -- 11.5.1.3 Phosphorus -- 11.5.2 Hiatuses and the Way Forward -- References -- Chapter 12: Soil-Vegetation Interactions in Amazonia -- 12.1 Historical Perspective -- 12.2 The Geology and Geomorphology of the Amazon Basin -- 12.3 Soils and Nutrient Cycling in Amazonian Forests. , 12.4 Influence of Soils on Forest Species Composition, Structure, and Dynamics -- 12.4.1 Species Composition -- 12.4.2 Forest Dynamics -- 12.4.3 Forest Biomass -- References -- Chapter 13: Fires in Amazonia -- 13.1 Introduction -- 13.1.1 Fire Incidence -- 13.1.2 Fire Usage in Amazonia -- 13.1.3 Fire, Land Use, and Land Cover -- 13.1.4 Fire, Climate Seasonality, and Droughts -- 13.2 Fire Impacts -- 13.2.1 Extent of Burned Areas -- 13.2.2 Impact Fires on the Structure, Composition, and Carbon Stocks of Forests -- 13.3 Modelling Fire Occurrence in Amazonia -- 13.4 Conclusions -- Box 1: Challenges for Estimating Burnt Forest Areas in the Satellite Era -- References -- Chapter 14: Modelling Amazonian Carbon Budgets and Vegetation Dynamics in a Changing Climate -- 14.1 Introduction -- 14.2 DGVMs for the Amazon -- 14.2.1 Soil-Plant Water Relations -- 14.2.2 Direct Effects of Water Stress on GPP and Transpiration -- 14.2.3 Temperature Dependence of GPP -- 14.2.4 Temperature Dependence of Respiration -- 14.2.5 CO2 and Nutrient Sensitivity of Amazon Forest Productivity -- 14.2.6 Functional Types Versus Continuous Traits -- 14.2.7 Allocation of Primary Productivity over Vegetation Components -- 14.2.8 Modelling Biomass: Demography of Vegetation Carbon, Mortality, Disturbance, Dispersal, and Recruitment -- 14.2.9 The Role of Fire in Natural Forests -- 14.3 Conclusion -- References -- Part V: Integrating Considerations Between Biophysical and Social Aspects -- Chapter 15: Land Use, Land Cover and Land Use Change in the Brazilian Amazon (1960-2013) -- 15.1 Introduction -- 15.2 Data and Information Sources Available on Land Use and Land Cover (LULC) Change -- 15.3 Occupation of Brazilian Amazon: Drivers and Trends in Deforestation -- 15.4 The Impacts of Land Use Change -- 15.5 Conclusions -- References. , Chapter 16: The Impact of Land Use on Carbon Stocks and Fluxes in Brazilian Amazonia: Implications for Policy.
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  • 2
    Publication Date: 2023-07-19
    Description: We investigated the role of whitesand ecosystems (WSEs) in blackwater formation in the Rio Negro basin in order to develop novel constraints for the terrestrial carbon export from land to ocean. Orbitrap mass spectrometry, a kind of ultrahigh resolution technique (FT-MS), allows to resolve thousand of individual molecular features per DOM sample. Precise determination of exact mass allows the assignment of molecular formulae to these features. We therefore identified molecular markers using Orbitrap mass spectrometry from dissolved organic carbon (DOC) of ground- and surface waters in two contrasting WSEs feeding Rio Negro tributaries and compared them with known Rio Negro markers. One tributary was fed by a whitesand riparian valley connected to a terra firme plateau, while the other was fed by a typical upland whitesand Campina. We sampled at the end of October and beginning of November 2017. "Data Set S1", an .xlsx file, contains the crosstab (samples in columns, formulae in rows) of all molecular formulae, the DOM index data (chemical indices calculated from the formula data), ecosystem averages (averages across DOM samples from the same ecosystem), ecosystem fingerprint assignments (indicative formulae per ecosystem type as assessed by t-tests, i.e., significantly "enriched" formulae based on ion abundance data), Rio Negro marker overlap (comparison of fingerprints with two sets of published Rio Negro markers from Gonsior et al. 2016 (doi:10.5194/bg-13-4279-2016) and Simon et al. 2019 (doi:10.1016/j.orggeochem.2019.01.013), and evaluation of structural data from PubChem (for those nine WSE formulae that showed consistent matching with Rio Negro markers). "Data Set S2", also an .xlsx file, contains the merged crosstab that was used for a general dataset comparison of whitesand DOM and the two openly available Rio Negro datasets. "Data Set S3" is a .docx file containing the list of structure suggestions for nine potential whitesand Rio Negro markers from PubChem, including the structural formulae (which are not provided in "Data Set S1").
    Keywords: Age; Age, 14C calibrated (Graven et al. 2015); ALTITUDE; Amazon; Blackwater; Calculated after Dansgaard (1964); Campina; Carbon, organic, dissolved; C export; Comment; Conductivity, electrical; Cuieiras; Date/Time of event; Deuterium excess; Dissolved Organic Matter; DOC; DOM; Event label; Extraction efficiency; Fraction modern carbon; Geology, comment; Latitude of event; Location; Longitude of event; Optional event label; P2; P4; P5; P6; P7; pH; PP1; PP2; PR10; PR11; PR6; PR7; PR8; PR9; PT6; RA; RC; Rio_Negro-P2; Rio_Negro-P4; Rio_Negro-P5; Rio_Negro-P6; Rio_Negro-P7; Rio_Negro-PP1; Rio_Negro-PP2; Rio_Negro-PR10; Rio_Negro-PR11; Rio_Negro-PR6; Rio_Negro-PR7; Rio_Negro-PR8; Rio_Negro-PR9; Rio_Negro-PT6; Rio_Negro-RA; Rio_Negro-RC; Rio Negro; Sample ID; tropics; Type; Water level; Whitesand; Δ14C; δ18O; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 248 data points
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  • 3
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Wetlands of the Amazon River basin are globally significant sources of atmospheric methane. Satellite remote sensing (passive and active microwave) of the temporally varying extent of inundation and vegetation was combined with field measurements to calculate regional rates of methane emission for Amazonian wetlands. Monthly inundation areas for the fringing floodplains of the mainstem Solimões/Amazon River were derived from analysis of the 37 GHz polarization difference observed by the Scanning Multichannel Microwave Radiometer from 1979 to 1987. L-band synthetic aperture radar data (Japanese Earth Resources Satellite-1) were used to determine inundation and wetland vegetation for the Amazon basin (〈500 m elevation) at high (May–June 1996) and low water (October 1995). An extensive set of measurements of methane emission is available from the literature for the fringing floodplains of the central Amazon, segregated into open water, flooded forest and floating macrophyte habitats. Uncertainties in the regional emission rates were determined by Monte Carlo error analyses that combined error estimates for the measurements of emission and for calculations of inundation and habitat areas. The mainstem Solimões/Amazon floodplain (54–70°W) emitted methane at a mean annual rate of 1.3 Tg C yr−1, with a standard deviation (SD) of the mean of 0.3 Tg C yr−1; 67% of this range in uncertainty is owed to the range in rates of methane emission and 33% is owed to uncertainty in the areal estimates of inundation and vegetative cover. Methane emission from a 1.77 million square kilometers area in the central basin had a mean of 6.8 Tg C yr−1 with a SD of 1.3 Tg C yr−1. If extrapolated to the whole basin below the 500 m contour, approximately 22 Tg C yr−1 is emitted; this mean flux has a greenhouse warming potential of about 0.5 Pg C as CO2. Improvement of these regional estimates will require many more field measurements of methane emission, further examination of remotely sensed data for types of wetlands not represented in the central basin, and process-based models of methane production and emission.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1573-5117
    Keywords: tropical lakes ; Amazonia ; nutrients ; seasonality ; fish kill
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The diel mixing patterns of two small floodplain lakes, Lago Jacaretinga in the Amazon drainage, and Lago Cristalino in the Rio Negro system, were investigated during both the high-water and low-water states of the Amazon River hydrograph. Measurements included temperature, oxygen, ammonia, phosphate, and chlorophyll. In both lakes thermal stratification developed during the day and was eroded at night. During the low-water period when the lakes were shallow, nocturnal circulation extended to the lake bottom, whereas when the lakes were deeper (greater than about 5 m), circulation did not reach the bottom and an anoxic hypolimnion developed. During the low-water period, percent of oxygen concentrations were relatively high but always less than saturation. Low oxygen concentrations were observed during the high-water period. At all times nocturnal mixing supplied a significant amount of oxygen to the lake ecosystems. Nighttime upward mixing of recycled nitrogen and phosphorus also appeared to be important nutrient sources for algal productivity.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1573-5117
    Keywords: tropical lakes ; Amazonia ; nutrients ; seasonality ; fish kill
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The diel mixing patterns of two small floodplain lakes, Lago Jacaretinga in the Amazon drainage, and Lago Cristalino in the Rio Negro system, were investigated during both the high-water and low-water states of the Amazon River hydrograph. Measurements included temperature, oxygen, ammonia, phosphate, and chlorophyll. In both lakes thermal stratification developed during the day and was eroded at night. During the low-water period when the lakes were shallow, nocturnal circulation extended to the lake bottom, whereas when the lakes were deeper (greater than about 5 m), circulation did not reach the bottom and an anoxic hypolimnion developed. During the low-water period, percent of oxygen concentrations were relatively high but always less than saturation. Low oxygen concentrations were observed during the high-water period. At all times nocturnal mixing supplied a significant amount of oxygen to the lake ecosystems. Nighttime upward mixing of recycled nitrogen and phosphorus also appeared to be important nutrient sources for algal productivity.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1572-9893
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography
    Notes: Abstract In this report the state of knowledge of sediment transport by rivers of the Amazon drainage basin is reviewed. On an annual basis the Amazon river transports about 1200×106 tons of sediment from the South American continent to the ocean, which puts it among the world's largest rivers in this respect. The main source of sediment is erosion in the Andes mountains and this material is progressively diluted with sediment poor runoff from lowland draining tributaries. Almost half of the Amazon river transport is attributable to one tributary, the Rio Madeira (488×106 t/y). The Rio Negro, which drains the N crystalline shield, has a comparable water discharge to the Rio Madeira, but only contributes 7×106 t/y. In general the sediments in transport are about 1% organic carbon by weight and this results in an annual particulate carbon to the oceans of 13×106 t/y. Total carbon transport, particulate plus dissolved, is about twice this amount.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1572-9893
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography
    Notes: Abstract Soil samples were collected on the floodplains of the Amazon River and its principal Brazilian tributaries during dry, early rising water, and early falling water periods. The concentrations of basic cations and pH in these alluvial soils were always higher than those in the more common “terra firme” soils while the concentrations of aluminum were generally lower. Among the alluvial soils, those from the main channel floodplain were generally higher in basic cations and pH, and lower in aluminum than those from the tribuary floodplains. The concentrations of basic cations in soils along the main channel floodplain decreased downstream. No significant difference was found in the levels of basic cations, pH, or aluminum between sampling periods.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1573-5117
    Keywords: tropical lakes ; Amazonia ; nutrients ; seasonality ; fish kill
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The diel mixing patterns of two small floodplain lakes, Lago Jacaretinga in the Amazon drainage, and Lago Cristalino in the Rio Negro system, were investigated during both the high-water and low-water states of the Amazon River hydrograph. Measurements included temperature, oxygen, ammonia, phosphate, and chlorophyll. In both lakes thermal stratification developed during the day and was eroded at night. During the low-water period when the lakes were shallow, nocturnal circulation extended to the lake bottom, whereas when the lakes were deeper (greater than about 5 m), circulation did not reach the bottom and an anoxic hypolimnion developed. During the low-water period, percent of oxygen concentrations were relatively high but always less than saturation. Low oxygen concentrations were observed during the high-water period. At all times nocturnal mixing supplied a significant amount of oxygen to the lake ecosystems. Nighttime upward mixing of recycled nitrogen and phosphorus also appeared to be important nutrient sources for algal productivity.
    Type of Medium: Electronic Resource
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