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Статті в журналах з теми "Marine organic matter"
Roelofs, G. J. "A GCM study of organic matter in marine aerosol and its potential contribution to cloud drop activation." Atmospheric Chemistry and Physics Discussions 7, no. 2 (April 27, 2007): 5675–700. http://dx.doi.org/10.5194/acpd-7-5675-2007.
Повний текст джерелаRoelofs, G. J. "A GCM study of organic matter in marine aerosol and its potential contribution to cloud drop activation." Atmospheric Chemistry and Physics 8, no. 3 (February 13, 2008): 709–19. http://dx.doi.org/10.5194/acp-8-709-2008.
Повний текст джерелаMiddelburg, Jack J., Tom Vlug, F. Jaco, and W. A. van der Nat. "Organic matter mineralization in marine systems." Global and Planetary Change 8, no. 1-2 (July 1993): 47–58. http://dx.doi.org/10.1016/0921-8181(93)90062-s.
Повний текст джерелаFuentes, E., H. Coe, D. Green, and G. McFiggans. "On the impacts of phytoplankton-derived organic matter on the properties of the primary marine aerosol – Part 2: Composition, hygroscopicity and cloud condensation activity." Atmospheric Chemistry and Physics 11, no. 6 (March 18, 2011): 2585–602. http://dx.doi.org/10.5194/acp-11-2585-2011.
Повний текст джерелаPassow, U., J. Dunne, J. W. Murray, L. Balistrieri, and A. L. Alldredge. "Organic carbon to 234Th ratios of marine organic matter." Marine Chemistry 100, no. 3-4 (August 2006): 323–36. http://dx.doi.org/10.1016/j.marchem.2005.10.020.
Повний текст джерелаTanoue, Eiichiro. "Dynamics and Characterization of Marine Organic Matter." Oceanography in Japan 13, no. 1 (2004): 7–23. http://dx.doi.org/10.5928/kaiyou.13.7.
Повний текст джерелаWada, Shigeki, Yuko Omori, Saki Yamashita, Yasuhito Hayashi, Takeo Hama, and Yasuhisa Adachi. "Aggregation of marine organic matter by bubbling." Journal of Oceanography 76, no. 4 (January 7, 2020): 317–26. http://dx.doi.org/10.1007/s10872-019-00538-1.
Повний текст джерелаFuentes, E., H. Coe, D. Green, and G. McFiggans. "On the impacts of phytoplankton-derived organic matter on the properties of the primary marine aerosol – Part 2: Composition, hygroscopicity and cloud condensation activity." Atmospheric Chemistry and Physics Discussions 10, no. 11 (November 4, 2010): 26157–205. http://dx.doi.org/10.5194/acpd-10-26157-2010.
Повний текст джерелаXue, Hai Tao, Guo Dong Mu, Shan Si Tian, and Shuang Fang Lu. "Gas Generation Regularities of Dissipated Soluble Organic Matter in Sichuan Basin." Advanced Materials Research 977 (June 2014): 308–11. http://dx.doi.org/10.4028/www.scientific.net/amr.977.308.
Повний текст джерелаO'Meara, Theresa, Emma Gibbs, and Simon F. Thrush. "Rapid organic matter assay of organic matter degradation across depth gradients within marine sediments." Methods in Ecology and Evolution 9, no. 2 (October 9, 2017): 245–53. http://dx.doi.org/10.1111/2041-210x.12894.
Повний текст джерелаДисертації з теми "Marine organic matter"
Nuwer, Jonathan Mark. "Organic matter preservation along a dynamic continental margin : form and fates of sedimentary organic matter /." Thesis, Connect to this title online; UW restricted, 2008. http://hdl.handle.net/1773/10999.
Повний текст джерелаBecker, Jamie William. "Microbial production and consumption of marine dissolved organic matter." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/80979.
Повний текст джерелаCataloged from PDF version of thesis.
Includes bibliographical references.
Marine phytoplankton are the principal producers of oceanic dissolved organic matter (DOM), the organic substrate responsible for secondary production by heterotrophic microbes in the sea. Despite the importance of DOM in marine food webs, details regarding how marine microbes cycle DOM are limited, and few definitive connections have been made between specific producers and consumers. Consumption is thought to depend on the source of the DOM as well as the identity of the consumer; however, it remains unclear how phytoplankton diversity and DOM composition are related, and the metabolic pathways involved in the turnover of DOM by different microbial taxa are largely unknown. The motivation for this thesis is to examine the role of microbial diversity in determining the composition, lability, and physiological consumption of marine DOM. The chemical composition of DOM produced by marine phytoplankton was investigated at the molecular level using mass spectrometry. Results demonstrate that individual phytoplankton strains release a unique suite of organic compounds. Connections between DOM composition and the phylogenetic identity of the producing organism were identified on multiple levels, revealing a direct relationship between phytoplankton diversity and DOM composition. Phytoplankton-derived DOM was also employed in growth assays with oligotrophic bacterioplankton strains to examine effects on heterotrophic growth dynamics. Reproducible responses ranged from suppressed to enhanced growth rates and cell yields, and depended both on the identity of the heterotroph and the source of the DOM. Novel relationships between specific bacterioplankton types and DOM from known biological sources were found, and targets for additional studies on reactive DOM components were identified. The physiology of DOM consumption by a marine Oceanospirillales strain was studied using a combined transcriptomic and untargeted metabolomic approach. The transcriptional response of this bacterium to Prochlorococcus-derived DOM revealed an increase in anabolic processes related to metabolism of carboxylic acids and glucosides, increased gene expression related to proteorhodopsin-based phototrophy, and decreased gene expression related to motility. Putative identification of compounds present in Prochlorococcus-derived DOM supported these responses. Collectively, these findings highlight the potential for linking detailed chemical analyses of labile DOM from a known biological source with bacterioplankton diversity and physiology.
by Jamie William Becker.
Ph.D.
Sosa, Oscar Abraham. "Microbial cycling of marine high molecular weight dissolved organic matter." Thesis, Massachusetts Institute of Technology, 2015. http://hdl.handle.net/1721.1/104332.
Повний текст джерелаCataloged from PDF version of thesis.
Includes bibliographical references.
Microorganisms play a central role mediating biogeochemical cycles in the ocean. Marine dissolved organic matter (DOM) - a reservoir of organic solutes and colloids derived from plankton is a major source of carbon, nutrients, and energy to microbial communities. The biological transformation and remineralization of DOM sustains marine productivity by linking the microbial food web to higher trophic levels (the microbial loop) and exerts important controls over the cycles of carbon and bioessential elements, such as nitrogen and phosphorus, in the sea. Yet insight into the underlying metabolism and reactions driving the degradation of DOM is limited partly because its exact molecular composition is difficult to constrain and appropriate microbial model systems known to decompose marine DOM are lacking. This thesis identifies marine microorganisms that can serve as model systems to study the metabolic pathways and biochemical reactions that control an important ecosystem function, DOM turnover. To accomplish this goal, bacterial isolates were obtained by enriching seawater in dilution-to-extinction culturing experiments with a natural source of DOM, specifically, the high molecular weight (HMW) fraction (>1 kDa nominal molecular weight) obtained by ultrafiltration. Because it is relatively easy to concentrate and it is fairly uniform in its chemical composition across the global ocean and other aquatic environments, HMW DOM has the potential to serve as a model growth substrate to study the biological breakdown of DOM. The phylogeny, genomes, and growth characteristics of the organisms identified through this work indicate that HMW DOM contains bioavailable substrates that may support widespread microbial populations in coastal and open-ocean environments. The availability of ecologically relevant isolates in culture can now serve to test hypothesis emerging from cultivation-independent studies pertaining the potential role of microbial groups in the decomposition of organic matter in the sea. Detailed studies of the biochemical changes exerted on DOM by selected bacterial strains will provide new insight into the processes driving the aerobic microbial food chain in the upper ocean.
by Oscar Abraham Sosa.
Ph. D.
De, la Fuente Gamero Patricia. "Dynamics of marine dissolved organic matter : ocean metabolism and climate transitions." Doctoral thesis, Universitat Politècnica de Catalunya, 2019. http://hdl.handle.net/10803/667649.
Повний текст джерелаEl Océano Global es el mayor reservorio de carbono y nutrientes que llegan al océano superior en escalas temporales de meses hasta 10.000 años. La disponibilidad de nutrientes es fundamental para la producción primaria y la concentración de carbono inorgánico dis suelto (DIC en inglés) en las aguas superficiales controla los cambios glacial-interglacial del CO2 atmosférico. La bomba de carbono microbiana (MCP en inglés) se refiere a la producción de compuestos refractarios de carbono orgánico disuelto (RDOC en inglés) a través de la actividad microbiana heterotrófica siendo un proceso que influye tanto en los nutrientes como en la disponibilidad de carbono. Las variaciones en el reservorio de RDOC afectan al almacenamiento de carbono a largo plazo en el océano, influyendo en el ciclo del carbono y el clima. El objetivo general de esta tesis es ampliar la comprensión de las conexiones entre la producción de RDOC por la MCP y el metabolismo oceánico (entendido como la producción comunitaria autótrofa neta del océano superior), prestando especial atención al papel de los procesos microbianos en las transiciones glacial - interglacial del sistema terrestre. La producción de RDOC por la MCP se infiere a través de la dependencia lineal de la materia orgánica disuelta fluorescente (FDOM, en inglés) con la utilización aparente de oxígeno (AOU, en inglés) y los nutrientes. Dicha relación depende del contenido preformado en las masas de agua. A partir de datos obtenidos a lo largo de 7.50N en el Océano Atlántico ecuatorial, se evalúa que variabilidad de la distribución de FDOM corresponde con producción in situ y cual a las propiedades del agua en origen. Se presenta una metodología objetiva y simple, no lineal y global para resolver la fracción no conservativa de la distribución de variables biogeoquímicas mediante el ajuste de modelos polinomiales en todo el espacio de temperatura y salinidad. Se evalúa la bondad del método para cada estrato de agua comparándolo con el enfoque tradicional, basado en la mezcla lineal y local de un máximo de tres masas de agua fuente. La nueva metodología distingue entre las contribuciones conservativas y no conservativas de las variables biogeoquímicas, proporciona información de procesos biogeoquímicos, relaciones estequiométricas y patrones de conectividad dentro de una región. Por primera vez, se formula una relación general entre FDOM tipo húmico y AOU en el Océano Atlántico ecuatorial, independiente de las masas de agua. Los resultados respaldan la idea de que el FDOM se produce principalmente in situ en el océano profundo. En la segunda parte de la tesis, se explora el papel del RDOC en las transiciones climáticas del cuaternario. Las transiciones glacial-interglacial se consideran estados funcionales del sistema terrestre, con diferentes condiciones energéticas en términos de conversión de la energía solar a través de la fotosíntesis. La capacidad del sistema oceánico para capturar y transformar la radiación solar incidente depende de la disponibilidad de DIC/nutrientes en el océano superior. El aporte de DIC/nutrientes por el Bucle Latitudinal (MOC, en inglés) y el reservorio de materia orgánica disuelta se evalúan a través de un modelo simple de dos cajas y de relajación de dos estados para el DIC/nutrientes en el océano superior. El modelo, inspirado en conceptos fisiológicos, considera que el océano superior cambia entre dos estados metabólicos diferentes, basal (glacial) y excitado (interglacial). El modelo reproduce la serie temporal de 𝐶���𝐶���𝐶���𝐶���2 atmosférico de los últimos 420 kyr, proporcionando la magnitud y dependencia temporal de la MOC y estableciendo restricciones en la producción primaria y la remineralización en el océano superior. El RDOC acumulado en el período glacial y su disponibilidad al final de este ciclo establece la intensidad metabólica del interglacial subsiguiente, constituyendo por tanto un componente central de la organización homeostática pulsante de la Tierra.
Morgan, Jessica A. "Bacterial Properties and Dissolved Organic Matter Distributions in the Black Sea." W&M ScholarWorks, 2003. https://scholarworks.wm.edu/etd/1539617804.
Повний текст джерелаCollins, James R. (James Robert). "The remineralization of marine organic matter by diverse biological and abiotic processes." Thesis, Massachusetts Institute of Technology, 2017. http://hdl.handle.net/1721.1/109053.
Повний текст джерелаCataloged from PDF version of thesis.
Includes bibliographical references.
While aerobic respiration is typically invoked as the dominant mass-balance sink for organic matter in the upper ocean, many other biological and abiotic processes can degrade particulate and dissolved substrates on globally significant scales. The relative strengths of these other remineralization processes - including mechanical mechanisms such as dissolution and disaggregation of sinking particles, and abiotic processes such as photooxidation - remain poorly constrained. In this thesis, I examine the biogeochemical significance of various alternative pathways of organic matter remineralization using a combination of field experiments, modeling approaches, geochemical analyses, and a new, high-throughput lipidomics method for identification of lipid biomarkers. I first assess the relative importance of particle-attached microbial respiration compared to other processes that can degrade sinking marine particles. A hybrid methodological approach - comparison of substrate-specific respiration rates from across the North Atlantic basin with Monte Carlo-style sensitivity analyses of a simple mechanistic model - suggested sinking particle material was transferred to the water column by various biological and mechanical processes nearly 3.5 times as fast as it was directly respired, questioning the conventional assumption that direct respiration dominates remineralization. I next present and demonstrate a new lipidomics method and open-source software package for discovery and identification of molecular biomarkers for organic matter degradation in large, high-mass-accuracy HPLC-ESI-MS datasets. I use the software to unambiguously identify more than 1,100 unique lipids, oxidized lipids, and oxylipins in data from cultures of the marine diatom Phaeodactylum tricornutum that were subjected to oxidative stress. Finally, I present the results of photooxidation experiments conducted with liposomes - nonliving aggregations of lipids - in natural waters of the Southern Ocean. A broadband polychromatic apparent quantum yield (AQY) is applied to estimate rates of lipid photooxidation in surface waters of the West Antarctic Peninsula, which receive seasonally elevated doses of ultraviolet radiation as a consequence of anthropogenic ozone depletion in the stratosphere. The mean daily rate of lipid photooxidation (50 ± 11 pmol IP-DAG L⁻¹ d⁻¹, equivalent to 31 ± 7 [mu]g C m⁻³ d⁻¹) represented between 2 and 8 % of the total bacterial production observed in surface waters immediately following the retreat of the sea ice.
by James R. Collins.
Ph. D.
Brownawell, Bruce J. "The role of colloidal organic matter in the marine geochemistry of PCB's." Thesis, Massachusetts Institute of Technology, 1986. http://hdl.handle.net/1721.1/51453.
Повний текст джерелаMicrofiche copy available in Archives and Science.
Vita.
Bibliography: leaves 271-297.
by Bruce J. Brownawell.
Ph.D.
Arnarson, Thorarinn Sveinn. "Preservation of organic matter in marine sediments : a density fractionation and X-ray photoelectron spectroscopy approach /." Thesis, Connect to this title online; UW restricted, 2004. http://hdl.handle.net/1773/11050.
Повний текст джерелаBenitez-Nelson, Bryan C. "Marine sedimentary organic matter: delineation of marine and terrestrial sources through radiocarbon dating; and the role of organic sulfur in early petroleum generation." Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/58536.
Повний текст джерела"May 1996."
Includes bibliographical references (leaves 66-68).
This thesis details two years of research conducted with the guidance and support of three advisors: Dr. J. K. Whelan, Dr. J. S. Seewald and Dr. T. I. Eglinton. Each of the three chapters represents a different, self-contained research project. All of the projects are related to the organic geochemistry of marine sediments, however, this is a fairly encompassing area of study. Chapters 1 and 2 stem from the same experimental study -- the use of hydrous-pyrolysis to investigate mechanisms leading to the production of petroleum-related products during kerogen maturation. Chapter 3, on the other hand, utilizes a recently developed technique of isolating and AMS-14C dating individual compounds from complex sedimentary organic mixtures. The samples used in each investigation came from all over the world. The first two chapters utilize ancient marine sediment samples obtained from an outcrop in California (Chpts. 1 and 2) and from a well in Alabama (Chpt. 2). In contrast, recent marine sediment samples were obtained from the Arabian and Black Seas for the third chapter. Several preparative and analytical methods are common to all three studies. Nevertheless, each employ techniques totally unique from one another and from previous investigations. In Chapter 1, for example, X-ray absorption spectroscopy (XANES) is used to determine the speciation of organic sulfur present in kerogen, bitumen, and bulk sediment samples. While Chapter 3 represents the first study in which the "4C ages of individual, known hydrocarbon biomarkers are determined after isolation by Preparative Capillary Gas Chromatography (PCGC). The insights gained by these investigations are discussed in detail in the following chapters. The common thread between the three chapters is that the source of organic matter, the rate at which it is delivered to marine sediments and the depositional environment, all set the stage for kerogen formation and eventual petroleum generation.
by Bryan C. Benitez-Nelson.
M.S.
Elifantz, Hila. "Structure and function of microbial communities processing dissolved organic matter in marine environments." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 127 p, 2007. http://proquest.umi.com/pqdlink?did=1251898401&Fmt=7&clientId=79356&RQT=309&VName=PQD.
Повний текст джерелаКниги з теми "Marine organic matter"
Handa, Nobuhiko, Eiichiro Tanoue, and Takeo Hama, eds. Dynamics and Characterization of Marine Organic Matter. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-1319-1.
Повний текст джерелаVolkman, John K., ed. Marine Organic Matter: Biomarkers, Isotopes and DNA. Berlin/Heidelberg: Springer-Verlag, 2006. http://dx.doi.org/10.1007/b11682.
Повний текст джерелаTakeo, Hama, Tanoue Eiichiro, and Handa Nobuhiko 1932-, eds. Dynamics and characterization of marine organic matter. Tokyo: Terra Scientific Pub. Co., 2000.
Знайти повний текст джерелаGautier, Donald L. Relationship of organic matter and mineral diagenesis. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1985.
Знайти повний текст джерелаArtemʹev, V. E. Geochemistry of organic matter in river-sea systems. Dordrecht: Kluwer Academic Publishers, 1996.
Знайти повний текст джерелаBrownawell, Bruce J. The role of colloidal organic matter in the marine geochemistry of PCBs. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1986.
Знайти повний текст джерелаWaveren, I. M. van. Planktonic organic matter in surficial sediments of the Banda Sea (Indonesia): A palynological approach. [Utrecht: Faculteit Aardwetenschappen der Rijksuniversiteit te Utrecht, 1993.
Знайти повний текст джерелаK, Kharaka Yousif, Surdam Ronald C, and Society of Economic Paleontologists and Mineralogists., eds. Relationship of organic matter and mineral diagenesis: Lecture notes for short course no. 17. Tulsa, OK: SEPM, 1985.
Знайти повний текст джерелаGautier, Donald L. Relationship of organic matter and mineral diagenesis: Lecture notes for short course no.17 sponsored by the Society of Economic Paleontologists and Mineralogists. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1985.
Знайти повний текст джерелаLohrenz, Steven E. Primary production of particulate protien amino acids: Algal protein metabolism and its relationship to the composition of particulate organic matter. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1985.
Знайти повний текст джерелаЧастини книг з теми "Marine organic matter"
Romankevich, Evgeny, and Alexander Vetrov. "Organic Matter." In Encyclopedia of Marine Geosciences, 1–8. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_80-1.
Повний текст джерелаÁlvarez-Salgado, Xosé Antón, Mar Nieto-Cid, and Pamela E. Rossel. "Dissolved Organic Matter." In Marine Analytical Chemistry, 39–102. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-14486-8_2.
Повний текст джерелаTyson, Richard V. "Distribution of the Palynomorph Group: Phytoplankton Subgroup, Marine Prasinophyte Phycomata." In Sedimentary Organic Matter, 299–308. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0739-6_15.
Повний текст джерелаTyson, Richard V. "Distribution of the Palynomorph Group: Phytoplankton Subgroup, Marine Dinoflagellate Cysts (Dinocysts)." In Sedimentary Organic Matter, 285–98. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0739-6_14.
Повний текст джерелаValiela, Ivan. "Production: The Formation of Organic Matter." In Marine Ecological Processes, 35–60. New York, NY: Springer New York, 2015. http://dx.doi.org/10.1007/978-0-387-79070-1_2.
Повний текст джерелаMiddelburg, Jack J. "Organic Matter is more than CH2O." In Marine Carbon Biogeochemistry, 107–18. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10822-9_6.
Повний текст джерелаCurtis, Charles. "Mineralogical Consequences of Organic Matter Degradation in Sediments: Inorganic/Organic Diagenesis." In Marine Clastic Sedimentology, 108–23. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3241-8_6.
Повний текст джерелаRullkötter, Jürgen. "Organic Matter: The Driving Force for Early Diagenesis." In Marine Geochemistry, 129–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04242-7_4.
Повний текст джерелаHara, Seiko, and Isao Koike. "Dynamics of Organic Marine Aggregates: Nanometer-Colloids to Marine Snow." In Dynamics and Characterization of Marine Organic Matter, 277–98. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-1319-1_14.
Повний текст джерелаCanfield, Donald E. "Organic Matter Oxidation in Marine Sediments." In Interactions of C, N, P and S Biogeochemical Cycles and Global Change, 333–63. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-76064-8_14.
Повний текст джерелаТези доповідей конференцій з теми "Marine organic matter"
Raja, M., and A. Rosell-Melé. "Global Drivers of Marine Organic Matter to Deep Sea Sediments." In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902876.
Повний текст джерелаLi, Z., S. George, and H. Sadatzki. "Organic Matter Input to Marine Sediments off East Antarctica." In 30th International Meeting on Organic Geochemistry (IMOG 2021). European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202134208.
Повний текст джерелаBruni, E., T. M. Blattmann, N. Haghipour, D. B. Montlucon, and T. I. Eglinton. "Organic Matter Distribution is Controlled by Sedimentological Parameters in Marine Oxygen Minimum Zone." In 30th International Meeting on Organic Geochemistry (IMOG 2021). European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202134222.
Повний текст джерелаJarassova, Tolganay, and Mehmet Altunsoy. "Organic Geochemical Characteristics of Core Samples from Central Primorsk-Emba Province, Precaspian Basin, Kazakhstan." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207044-ms.
Повний текст джерелаJarassova, Tolganay, and Mehmet Altunsoy. "Organic Geochemical Characteristics of Core Samples from Central Primorsk-Emba Province, Precaspian Basin, Kazakhstan." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207044-ms.
Повний текст джерелаLupascu, Angela. "CONSIDERATIONS CONCERNING THE ORGANIC MATTER FROM OAS MOUNTAINS REPRESENTATIVE SOILS (EASTERN CARPHATIANS, ROMANIA)." In 14th SGEM GeoConference on WATER RESOURCES. FOREST, MARINE AND OCEAN ECOSYSTEMS. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b32/s13.007.
Повний текст джерелаGhervase, Luminita. "SPATIAL ARRANGEMENT FLAWS IN RURAL AREAS EVIDENCED BY DISSOLVED ORGANIC MATTER DISTRIBUTION IN GROUNDWATER." In 14th SGEM GeoConference on WATER RESOURCES. FOREST, MARINE AND OCEAN ECOSYSTEMS. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b31/s12.081.
Повний текст джерелаFreitas, F. S., P. A. Pika, J. Holtvoeth, S. Arndt, and R. D. Pancost. "Global Patterns of Reactivity and Sources of Organic Matter in Marine Sediments: A Coupled Model and Lipid Biomarker Approach." In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902676.
Повний текст джерелаYamaguchi, Yasuhiko T., Matthew D. Mccarthy, Chikage Yoshimizu, Ichiro Tayasu, Keisuke Koba, and Kazuhide Hayakawa. "Distribution of “Minor” Amino Acids Enantiomers in Dissolved Organic Matter in Marine vs. Inland Waters." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2962.
Повний текст джерелаMoldoveanu, Aurelia�Manuela. "THE�DYNAMICS�OF�MARINE�BACTERIONEUSTON��IN�LABORATORY�MICROCOSMS:�2.�THE�INFLUENCE�OF�ORGANIC�MATTER�ADDITION." In SGEM2012 12th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2012. http://dx.doi.org/10.5593/sgem2012/s14.v3011.
Повний текст джерелаЗвіти організацій з теми "Marine organic matter"
Landry, M. R. Utilization, cycling and vertical transport of particulate organic matter in the coastal marine environment. Office of Scientific and Technical Information (OSTI), January 1992. http://dx.doi.org/10.2172/7007590.
Повний текст джерелаPaytan, Adina. Organic Matter Composition, Recycling Susceptibility, and the Effectiveness of the Biological Pump – An Evaluation Using NMR Spectra of Marine Plankton. Office of Scientific and Technical Information (OSTI), February 2014. http://dx.doi.org/10.2172/1120791.
Повний текст джерелаLandry, M. R. Utilization, cycling and vertical transport of particulate organic matter in the coastal marine environment. Final project report, November 15, 1987--May 14, 1992. Office of Scientific and Technical Information (OSTI), October 1992. http://dx.doi.org/10.2172/10184183.
Повний текст джерелаBurdige, David J. Colored Dissolved Organic Matter in Sediments and Seagrass Beds and Its Impact on Benthic Optical Properties of Shallow Water Marine Environments - Data Analysis and Synthesis, and Student Support. Fort Belvoir, VA: Defense Technical Information Center, September 2004. http://dx.doi.org/10.21236/ada426835.
Повний текст джерелаBurdige, David J. Colored Dissolved Organic Matter in Sediments and Seagrass Beds and its Impact on Benthic Optical Properties of Shallow Water Marine Environments - Data Analysis and Synthesis, and Student Support. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada619752.
Повний текст джерелаBurdige, David J. Colored Dissolved Organic Matter in Sediments and Seagrass Beds and its Impact on Benthic Optical Properties of Shallow Water Marine Environments - Data Analysis and Synthesis, and Student Support. Fort Belvoir, VA: Defense Technical Information Center, September 2002. http://dx.doi.org/10.21236/ada626578.
Повний текст джерелаJahnke, R. A. Sea floor cycling of organic matter in the continental margin of the mid-Atlantic Bight. Final report, May 1, 1995--April 30, 1998. Office of Scientific and Technical Information (OSTI), December 1998. http://dx.doi.org/10.2172/329503.
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