Search results for "lcsh:QH501-531"

showing 10 items of 31 documents

Nitrous oxide emission budgets and land-use-driven hotspots for organic soils in Europe

2014

Organic soils are a main source of direct emissions of nitrous oxide (N2O), an important greenhouse gas (GHG). Observed N2O emissions from organic soils are highly variable in space and time, which causes high uncertainties in national emission inventories. Those uncertainties could be reduced when relating the upscaling process to a priori-identified key drivers by using available N2O observations from plot scale in empirical approaches. We used the empirical fuzzy modelling approach MODE to identify main drivers for N2O and utilize them to predict the spatial emission pattern of European organic soils. We conducted a meta-study with a total amount of 659 annual N2O measurements, which was…

N-DEPOSITION1171 GeosciencesPeat010504 meteorology & atmospheric sciencesGRASSLANDWater tableeducationlcsh:LifeGreenhouse gas inventorySoil scienceAtmospheric sciences01 natural sciencesGrasslandSoil pHlcsh:QH540-549.5media_common.cataloged_instanceAGRICULTURAL SOILSEuropean unionEcology Evolution Behavior and Systematics1172 Environmental sciences0105 earth and related environmental sciencesEarth-Surface Processesmedia_commongeographyPOLICY SUPPORT4112 Forestrygeography.geographical_feature_categoryCH4lcsh:QE1-996.504 agricultural and veterinary sciences15. Life on landWATER-TABLEPEAT SOILSlcsh:Geologylcsh:QH501-53113. Climate actionGreenhouse gasSoil waterNORTHERN PEATLANDS040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceCO2lcsh:EcologyN2O FLUXES
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Modelling biogeochemical processes in sediments from the north-western Adriatic Sea: response to enhanced particulate organic carbon fluxes

2018

This work presents the result of a study carried out in the north-western Adriatic Sea, by combining two different types of biogeochemical models with field sampling efforts. A longline mussel farm was taken as a local source of perturbation to the natural particulate organic carbon (POC) downward flux. This flux was first quantified by means of a pelagic model of POC deposition coupled to sediment trap data, and its effects on sediment bioirrigation capacity and organic matter (OM) degradation pathways were investigated constraining an early diagenesis model by using original data collected in sediment porewater. The measurements were performed at stations located inside and outside the ar…

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean Atmosphere0106 biological sciencesSettore BIO/07 - EcologiaBiogeochemical cycle010504 meteorology & atmospheric sciencesMARINE-SEDIMENTSEARLY-DIAGENESISlcsh:LifeMEDITERRANEAN LAGOONMUSSEL CULTURE01 natural sciencesNITROGEN DYNAMICS[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrylcsh:QH540-549.5Dissolved organic carbon[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentbiogeochemistry marine sediments carbon fluxesOrganic matter14. Life underwaterDYNAMIC ENERGY BUDGETComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesEarth-Surface Processeschemistry.chemical_classificationTotal organic carbonSULFATE REDUCTION010604 marine biology & hydrobiologylcsh:QE1-996.5BioirrigationBiogeochemistrySedimentWATER INTERFACEMusselDYNAMIC ENERGY BUDGET EARLY-DIAGENESIS WATER INTERFACE MUSSEL CULTURE MEDITERRANEAN LAGOON NITROGEN DYNAMICS COASTAL SEDIMENTS SULFATE REDUCTION NUTRIENT DYNAMICS MARINE-SEDIMENTSNUTRIENT DYNAMICSlcsh:Geologylcsh:QH501-531Oceanographychemistry13. Climate actionEnvironmental sciencelcsh:EcologyCOASTAL SEDIMENTSDYNAMIC ENERGY BUDGET; EARLY-DIAGENESIS; WATER INTERFACE; MUSSEL CULTURE; MEDITERRANEAN LAGOON; NITROGEN DYNAMICS; COASTAL SEDIMENTS; SULFATE REDUCTION; NUTRIENT DYNAMICS; MARINE-SEDIMENTS
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Assessing the potential long-term increase of oceanic fossil fuel CO2 uptake due to CO2-calcification feedback

2007

International audience; Plankton manipulation experiments exhibit a wide range of sensitivities of biogenic calcification to simulated anthropogenic acidification of the ocean, with the "lab rat" of planktic calcifiers, Emiliania huxleyi apparently not representative of calcification generally. We assess the implications of this observational uncertainty by creating an ensemble of realizations of an Earth system model that encapsulates a comparable range of uncertainty in calcification response to ocean acidification. We predict that a substantial reduction in marine carbonate production is possible in the future, with enhanced ocean CO2 sequestration across the model ensemble driving a 4?1…

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmospherelcsh:QE1-996.5fungilcsh:Life[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph][ PHYS.ASTR.CO ] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO][SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentlcsh:Geologylcsh:QH501-531[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]lcsh:QH540-549.5[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentlcsh:Ecology[ SDU.ASTR ] Sciences of the Universe [physics]/Astrophysics [astro-ph]
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The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a …

2007

Abstract. Sponges (phylum Porifera) had been considered as an enigmatic phylum, prior to the analysis of their genetic repertoire/tool kit. Already with the isolation of the first adhesion molecule, galectin, it became clear that the sequences of the sponge cell surface receptors and those of the molecules forming the intracellular signal transduction pathways, triggered by them, share high similarity to those identified in other metazoan phyla. These studies demonstrated that all metazoan phyla, including the Porifera, originate from one common ancestor, the Urmetazoa. The sponges evolved during a time prior to the Ediacaran-Cambrian boundary (542 million years ago (myr)). They appeared du…

biologyPhylum[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmospherelcsh:QE1-996.5lcsh:Lifemyrbiology.organism_classification[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph][SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentSuberites domunculaIntracellular signal transductionlcsh:GeologySpongelcsh:QH501-531Body planSponge spiculeEvolutionary biology[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]lcsh:QH540-549.5Botany[SDU.STU] Sciences of the Universe [physics]/Earth Scienceslcsh:EcologyLiving fossilEcology Evolution Behavior and SystematicsEarth-Surface Processes
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Lignin oxidation products in soil, dripwater and speleothems from four different sites in New Zealand

2020

Lignin oxidation products (LOPs) are widely used as vegetation proxies in climate archives, such as sediment and peat cores. The total LOP concentration, Σ8, provides information on the abundance of vegetation, while the ratios C/V and S/V of the different LOP groups also provide information on the type of vegetation. Recently, LOP analysis has been successfully applied to speleothem archives. However, there are many open questions concerning the transport and microbial degradation of LOPs on their way from the soil into the cave system. These processes could potentially alter the original source-dependent LOP signals, in particular the C/V and S/V ratios, and thus complicate their interpre…

lcsh:Geologylcsh:QH501-53113. Climate actionlcsh:QH540-549.5lcsh:QE1-996.5lcsh:LifeF800lcsh:Ecology15. Life on land
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Quantification of lignin oxidation products as vegetation biomarkers in speleothems and cave drip water

2018

Here we present a sensitive method to analyze lignin oxidation products (LOPs) in speleothems and cave drip water to provide a new tool for paleo-vegetation reconstruction. Speleothems are valuable climate archives. However, compared to other terrestrial climate archives, such as lake sediments, speleothems contain very little organic matter. Therefore, very few studies on organic biomarkers in speleothems are available. Our new sensitive method allows us to use LOPs as vegetation biomarkers in speleothems. Our method consists of acid digestion of the speleothem sample followed by solid-phase extraction (SPE) of the organic matter. The extracted polymeric lignin is degraded in a microwave-a…

lcsh:Geologylcsh:QH501-53113. Climate actionlcsh:QH540-549.5lcsh:QE1-996.5lcsh:Lifelcsh:Ecology15. Life on land
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Characterisation of NO production and consumption: new insights by an improved laboratory dynamic chamber technique

2014

Biogenic NOx emissions from natural and anthropogenically influenced soils are currently estimated to amount to 9 Tg a−1, hence a significant fraction of global NOx emissions (45 Tg a−1). During the last three decades, a large number of field measurements have been performed to quantify biogenic NO emissions. To study biogenic NO emissions as a function of soil moisture, soil temperature, and soil nutrients, several laboratory approaches have been developed to estimate local/regional NO emissions by suitable upscaling. This study presents an improved and automated laboratory dynamic chamber system (consisting of six individual soil chambers) for investigation and quantification of all quant…

lcsh:Geologylcsh:QH501-531lcsh:QH540-549.5lcsh:QE1-996.5lcsh:Lifelcsh:EcologyBiogeosciences
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Applicability and consequences of the integration of alternative models for CO2 transfer velocity into a process-based lake model

2019

Freshwater lakes are important in carbon cycling, especially in the boreal zone where many lakes are supersaturated with the greenhouse gas carbon dioxide (CO2) and emit it to the atmosphere, thus ventilating carbon originally fixed by the terrestrial system. The exchange of CO2 between water and the atmosphere is commonly estimated using simple wind-based parameterizations or models of gas transfer velocity (k). More complex surface renewal models, however, have been shown to yield more correct estimates of k in comparison with direct CO2 flux measurements. We incorporated four gas exchange models with different complexity into a vertical process-based physico-biochemical lake model, MyLak…

lcsh:Geologylcsh:QH501-531lcsh:QH540-549.5lcsh:QE1-996.5lcsh:Lifelcsh:EcologyBiogeosciences
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Revisiting the disappearance of terrestrial dissolved organic matter in the ocean: a δ13C study

2014

Organic carbon (OC) depleted in 13C is a widely used tracer for terrestrial organic matter (OM) in aquatic systems. Photochemical reactions can, however, change δ13C of dissolved organic carbon (DOC) when chromophoric, aromatic-rich terrestrial OC is selectively mineralized. We assessed the robustness of the δ13C signature of DOC (δ13CDOC) as a tracer for terrestrial OM by estimating its change during the photobleaching of chromophoric DOM (CDOM) from 10 large rivers. These rivers cumulatively account for approximately one-third of the world's freshwater discharge to the global ocean. Photobleaching of CDOM by simulated solar radiation was associated with the photochemical mineralization of…

lcsh:Geologylcsh:QH501-531lcsh:QH540-549.5lcsh:QE1-996.5lcsh:Lifelcsh:EcologyBiogeosciences
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Diversity and mineral substrate preference in endolithic microbial communities from marine intertidal outcrops (Isla de Mona, Puerto Rico)

2017

14 pages; International audience; Endolithic microbial communities are prominent features of intertidal marine habitats, where they colonize a variety of substrates, contributing to their erosion. Almost 2 centuries worth of naturalistic studies focused on a few true-boring (euendolithic) phototrophs, but substrate preference has received little attention. The Isla de Mona (Puerto Rico) intertidal zone offers a unique setting to investigate substrate specificity of endolithic communities since various phosphate rock, limestone and dolostone outcrops occur there. High-throughput 16S rDNA genetic sampling, enhanced by targeted cultivation, revealed that, while euendolithic cyanobacteria were …

lcsh:Geologylcsh:QH501-531lcsh:QH540-549.5lcsh:QE1-996.5lcsh:Lifelcsh:Ecology14. Life underwater[ SDV.MP.BAC ] Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology[ SDV.IB.BIO ] Life Sciences [q-bio]/Bioengineering/Biomaterials
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