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1

Jones, Karen Patricia Nievergelt. "Studies of fine-grained, deep sea sediments." Thesis, University of Cambridge, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.238138.

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2

Tangherlini, Michael. "Microbial diversity and gene flow in deep-sea sediments." Doctoral thesis, Università Politecnica delle Marche, 2014. http://hdl.handle.net/11566/242906.

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La metagenomica ha permesso lo studio della diversità degli organismi non coltivabili e il loro ruolo nei vari ecosistemi tra cui suoli e sedimenti marini. acque interne e di oceano aperto. L’analisi della diversità attraverso gli approcci metagenomici è basata sull’estrazione del DNA genomico assumendo che questo sia completamente associato a biomassa vivente. Tuttavia, recenti studi hanno dimostrato che il metagenoma completo di ogni campione ambientale è costituito da pool differenti, tra cui: ,quello dei virus, quello associato a biomassa microbica e quello associato a biomassa non v
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3

Laurila, Tea Elisa. "The Metalliferous Sediments of the Atlantis II Deep (Red Sea)." Thesis, Université d'Ottawa / University of Ottawa, 2015. http://hdl.handle.net/10393/32229.

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The Atlantis II Deep is a location of modern submarine hydrothermal activity along the slowly spreading Red Sea rift axis. Venting of high-temperature hydrothermal fluids, similar to those associated with black smokers, takes place in a brine pool and has led to the accumulation of 90 Mt (dry, salt free) of stratiform, metalliferous sediment. The conditions of mineralization are unique in the modern oceans, but have been widely suggested as a possible analog of some important ancient stratiform base metal ore deposits. This study shows that many of the proposed genetic models for these ancient
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4

Scutton, Ian. "Trace metal and organic matter diagenesis in deep-sea sediments." Thesis, University of Liverpool, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.284175.

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5

Ståhl, Henrik. "Carbon-cycling in deep-sea and contrasting continental margin sediments /." Göteborg : Göteborg university, 2001. http://catalogue.bnf.fr/ark:/12148/cb401108738.

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6

Telling, Jon. "The geomicrobiology of deep-sea sediments on the Mid-Atlantic Ridge." Thesis, University of Bristol, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.393001.

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7

Bijaksana, Satria. "Magnetic anisotropy and correction of paleomagnetic inclination shallowing in deep-sea sediments." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1996. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq25768.pdf.

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8

Thomas, A. R. "Glacial-interglacial variations in the geochemistry of North Atlantic deep-sea sediments." Thesis, University of Liverpool, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.382148.

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9

Mutch, Thomas J. "Magnetic properties of quaternary deep-sea sediments : use as proxies for dust inputs?" Thesis, University of East Anglia, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.365095.

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10

West, Fraser James Craig. "Interactions between marine benthic invertebrates and sediments in intertidal and deep sea environments." Thesis, University of Glasgow, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.395057.

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11

Brothers, Richard John. "The mechanical formation of vein structures as fluid flow pathways in Peru margin sediments and the Monterey formation, California." Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262451.

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12

Rashid, Harunur. "The deep-sea record of rapid late pleistocene paleoclimate change and ice-sheet dynamics in Labrador sea sediments /." Thesis, McGill University, 2002. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=38540.

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Thirty eight piston cores and numerous seismic profiles collected by two R/V Marion Dufresne and several CSS Hudson cruises were examined and cores from other cruises reinterpreted in the course of this study of Late Pleistocene ice-rafting events (Heinrich events) in the Labrador Sea.<br>In the northwestern Labrador Sea, close to the margin of the former Laurentide Ice Sheet, Heinrich layers are unusually thick. Thicknesses of up to 4.8 m result from deposition from nepheloid-flows and low-density turbidity flows and from iceberg melting. Heinrich layers formed in three stages, explained by a
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13

Burke, Ian Terence. "Ocean-climate processes recorded in holocene laminated sediments from the Gotland Deep, Baltic Sea." Thesis, University of Southampton, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.392644.

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14

Grayson, Richard Philip. "Excess ²²⁶Ra chronology of lake and deep-sea sediments : an investigation of controls over sediment-water transfer." Thesis, University of Liverpool, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.426105.

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15

Yucel, Mustafa. "New perspectives in sulfur-iron cycling at the ocean-seafloor interface the Black Sea sediments and deep-sea hydrothermal vents /." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 203 p, 2010. http://proquest.umi.com/pqdweb?did=1997524241&sid=5&Fmt=2&clientId=8331&RQT=309&VName=PQD.

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16

Gontikaki, Evangelia. "Carbon cycling in continental slope sediments : the role of benthic communities." Thesis, University of Aberdeen, 2010. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=128351.

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Previous pulse-chase experiments have revealed a wide diversity of benthic response patterns to organic matter (OM) input depending on environmental setting, benthic community structure and experimental conditions i.e. quantity and quality of the added OM.  However, the mechanisms and interaction of environmental and biological factors that produce an observed response pattern are poorly understood. The present thesis set out to improve our current understanding on the set of parameters that determine benthic response patterns.  The core of this study was based on two pulse-chase experiments i
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17

BALDRIGHI, ELISA. "Macrofauna biodiversity and ecosystem functioning in the deep-sea. Mediterranean sediments: analysis at different spatial scales." Doctoral thesis, Università Politecnica delle Marche, 2013. http://hdl.handle.net/11566/242688.

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L’obiettivo principale della mia tesi di dottorato è stato quello di investigare le relazioni tra la biodiversità della macrofauna profonda del Mar Mediterraneo ed il funzionamento eco sistemico (BEF). Tale studio è stato svolto considerando differenti scale spaziali d’indagine, i) da centinaia di metri a diversi chilometri; ii) centinaia di chilometri e iii) migliaia di chilometri, e comprendendo sistemi di scarpata continentale con caratteristiche ambientali differenti. Sono state testate le seguenti ipotesi: 1) vi è una relazione significativa tra la biodiversità della macrofauna profo
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18

Bellew, Glen M. "Consolidation properties, stress history, and modeling of pore pressures for deep sea sediments at the Nankai Trough /." free to MU campus, to others for purchase, 2004. http://wwwlib.umi.com/cr/mo/fullcit?p1421111.

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19

Perks, Helen M. "Climatic and oceanographic controls on the burial and preservation of organic matter in equatorial Pacific deep-sea sediments /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1999. http://wwwlib.umi.com/cr/ucsd/fullcit?p3035921.

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20

Paul, Sophie Anna Luise [Verfasser], Andrea [Akademischer Betreuer] Koschinsky, Andrea [Gutachter] Koschinsky, Michael [Gutachter] Bau, Sabine [Gutachter] Kasten, and Thomas [Gutachter] Kuhn. "Biogeochemistry of Pacific deep-sea sediments and potential impacts of deep-sea polymetallic nodule mining / Sophie Anna Luise Paul ; Gutachter: Andrea Koschinsky, Michael Bau, Sabine Kasten, Thomas Kuhn ; Betreuer: Andrea Koschinsky." Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2019. http://d-nb.info/1190888157/34.

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21

Menendez, Gamella Amaya. "Controls on the composition and extraction of rare earth elements and yttrium (REY) in deep sea polymetallic nodules and sediments." Thesis, University of Southampton, 2017. https://eprints.soton.ac.uk/421113/.

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Rising demand for metals is driving a search for new mineral resources and mining of seafloor deposits is likely to commence in the next few years. These include polymetallic nodules and crusts that are highly enriched in Mn, Co, Ni, Cu, Mo, Li and Te, and deep-sea clays that can contain high concentrations of the rare earth elements and yttrium (REY). The potential environmental impacts of mining these deposits are, however, poorly constrained and a better understanding of the processes that control metal enrichment in marine resources is essential. In support of this, I have undertaken detai
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22

Hoffmann, Katy Verfasser], Antje [Akademischer Betreuer] [Gutachter] [Boetius, and Ulrich [Gutachter] Fischer. "Identity and function of key bacterial groups in Arctic deep-sea surface sediments / Katy Hoffmann ; Gutachter: Antje Boetius, Ulrich Fischer ; Betreuer: Antje Boetius." Bremen : Staats- und Universitätsbibliothek Bremen, 2017. http://d-nb.info/1140581767/34.

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23

Kallweit, Wiebke [Verfasser], Matthias [Akademischer Betreuer] Zabel, and Thomas [Akademischer Betreuer] Wagner. "Terrigenous climate signals in deep-sea sediments: Insights from the inorganic and organic geochemistry / Wiebke Kallweit. Gutachter: Matthias Zabel ; Thomas Wagner. Betreuer: Matthias Zabel." Bremen : Staats- und Universitätsbibliothek Bremen, 2011. http://d-nb.info/1071898671/34.

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24

Domingues, Patrícia Maia. "Subaquatic sediments as sources of hydrocarbonoclastic and biosurfactant producing facultative anaerobic bacteria." Doctoral thesis, Universidade de Aveiro, 2018. http://hdl.handle.net/10773/22847.

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Doutoramento em Engenharia Química<br>Actualmente são conhecidas poucas estirpes bacterianas capazes de produzir biossurfactantes (BSFs) em condições de microaerobiose ou anaerobiose. Estas bactérias têm um papel importante não só em processos naturais (ex. formação de biofilmes ou de hidratos de gás), como podem ter diversas aplicações biotecnológicas (ex. estratégias de biorremediação e aplicações industriais). As bactérias produtoras de BSFs em condições de limitação de oxigénio, com capacidade para degradar hidrocarbonetos são de particular interesse para estratégias de biorremediaç
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25

Quéric, Nadia-Valérie [Verfasser], Wolf E. Akademischer Betreuer] Arntz, and Antje [Akademischer Betreuer] [Boetius. "Bacterial community patterns along small- and large-scale environmental radients in Arctic deep-sea sediments / Nadia-Valérie Quéric. Gutachter: Wolf E. Arntz ; Antje Boetius. Betreuer: Wolf E. Arntz." Bremen : Staats- und Universitätsbibliothek Bremen, 2008. http://d-nb.info/1072302683/34.

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26

Beckler, Jordon Scott. "The biogeochemical source and role of soluble organic-Fe(III) complexes in continental margin sediments." Diss., Georgia Institute of Technology, 2014. http://hdl.handle.net/1853/53016.

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In the past couple of decades, the discovery that iron is a limiting nutrient in large regions of the ocean has spurred much research into characterizing the biogeochemical controls on iron cycling. While Fe(II) is soluble at circumneutral pH, it readily oxidizes to Fe(III) in the presence of oxygen. Fe(III) is highly insoluble at circumneutral pH, presenting organisms with a bioavailability paradox stemming from the physiological challenge of using a solid phase mineral for assimilatory or dissimilatory purposes. Interestingly, dissolved organic-Fe(III) complexes can be stable in seawater
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27

Wu, Qiong. "New insights into the current- and past hydrology of the north-western subtropical Pacific Ocean over the past 25 kyr, based on investigations of the Nd isotopic composition of seawater and deep-sea sediments from the northern South China Sea." Thesis, Paris 11, 2014. http://www.theses.fr/2014PA112169/document.

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Le but de cette étude est de retracer l’évolution de l’hydrologie dans la partie occidentale de l’Océan Pacifique subtropical en utilisant le proxy εNd analysé sur les foraminifères et sur les oxydes de ferromanganèse authigéniques dans les sédiments. Ceux-ci proviennent de carottes sédimentaires prélevées au nord de la Mer de Chine du Sud (MCS). Avant d’utiliser l’εNd dans les sédiments profonds de la MCS, 16 profils d’eau de mer, collectés au nord de la MCS et dans le Mer des Philippines, ont été analysés afin d’établir la distribution d’εNd des masses d’eau dans l’ouest du Pacifique tropica
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28

Gao, Guohui. "Variations in the North African climate and in the hydrology of intermediate- and deep-water masses of the Mediterranean Sea during the late Quaternary : sedimentological, mineralogical and geochemical investigations of marine sediments." Electronic Thesis or Diss., université Paris-Saclay, 2024. http://www.theses.fr/2024UPASJ025.

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La circulation thermohaline méditerranéenne influence l'AMOC et les dépôts de sapropels. Cette étude examine les méthodes d'extraction des compositions isotopiques de Nd de l'eau de mer passée et la variabilité de la formation des eaux profondes pendant le dernier cycle climatique. Nos résultats montrent que l'εNd des foraminifères n'est pas affecté par la diagenèse des téphras. L'extraction séquentielle avec hydroxylamine hydrochloride donne des valeurs d'εNd cohérentes avec celles des foraminifères. L'εNd des eaux profondes de la mer Adriatique est resté constant durant les 16 derniers ka. L
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29

Volz, Jessica B. [Verfasser], Sabine [Akademischer Betreuer] Kasten, Sabine [Gutachter] Kasten, and Anton [Gutachter] Eisenhauer. "Impact of deep-sea mining on redox environment, biogeochemical processes and element fluxes within and from sediments of the Clarion-Clipperton Zone, Pacific Ocean / Jessica B. Volz ; Gutachter: Sabine Kasten, Anton Eisenhauer ; Betreuer: Sabine Kasten." Bremen : Staats- und Universitätsbibliothek Bremen, 2019. http://d-nb.info/1199537241/34.

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30

Alagarsamy, R. "Trace metals and organic matter diagenesis at the Oman Margin." Thesis, University of Liverpool, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243212.

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31

Shepel, Taras. "Obosnovanie parametrov kovšej zemlečerpatel'nych snarjadov dlja glubokovodnoj dobyči organo-mineral'nych osadkov." Doctoral thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2015. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-163765.

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The thesis is devoted to determining the parameters of the bucket to increase productivity of dredgers while mining deep-water organic-mineral sediments. It was achieved by increasing the fill factor through determining the rational geometrical parameters of the bucket. Analytical dependencies of the rational height and length of the bucket on the cutting parameters and physical-and-mechanical properties of the excavated sediments were determined. Expressions for defining forces while digging plasticity water-saturated soils were developed. Experimental investigations of the process of digging
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32

Länje, Marcus. "Cenozoic history of North Atlantic deep sea carbonate preservation." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-117984.

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Carbonate preservation in the oceans occurs at a depth called the carbonate compensation depth (CCD). The CCD is where the input rate of carbonate from the surface of the ocean is balanced by the dissolution rate. Factors controlling the CCD are the CO2 in the atmosphere, weathering, and productivity in the surface water, the depth of the lysocline and deep water currents (and their ocean circulation). Two previous studies have investigated the variation of the CCD through geologic time, one in the equatorial Pacific (Pälike et al., 2012) and the other compiled results from the Pacific, Atlant
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33

Main, Charlotte E. "On the fate of plumes from deep-sea oil well blowouts, and their effects on sediment communities." Thesis, University of Southampton, 2015. https://eprints.soton.ac.uk/378971/.

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Little is known about the fate of subsurface hydrocarbon plumes from prolonged oil well blowouts, and their effects on deep-sea sediment communities. As deepwater drilling expands in the Faroe-Shetland Channel (FSC), oil well blowouts are a possibility, and the complex ocean circulation of this region presents challenges to understanding possible subsurface oil pathways. Here, questions on the fate and effects of subsurface oil plumes were addressed with experiments and modelling. Experiments were performed on uncontaminated deep-sea sediments from a site remote from the FSC. A three dimension
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34

Thureborn, Petter. "Microbial Ecosystem Functions Along the Steep Oxygen Gradient of the Landsort Deep, Baltic Sea." Doctoral thesis, Södertörns högskola, Miljövetenskap, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:sh:diva-30910.

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Through complex metabolic interactions aquatic microbial life is essential as a driver of ecosystem functions and hence a prerequisite for sustaining plant and animal life in the sea and on Earth. Despite its ecological importance, infor­mation on the complexity of microbial functions and how these are related to environmental conditions is limited. Due to climate change and eutrophication, marine areas facing oxygen depletion are increasing and predicted to continue to do so in the future. Vertically steep oxygen gradients are particularly pronoun­ced in the Baltic Sea. In this thesis, theref
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35

Queiroz, Luciano Lopes. "Padrões de diversidade microbiana em sedimentos marinhos profundos influenciados por uma exsudação de asfalto." Universidade de São Paulo, 2015. http://www.teses.usp.br/teses/disponiveis/42/42132/tde-26082015-171953/.

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Sedimentos de mar profundo são ambientes estáveis e homogêneos, apesar disso, eles apresentam uma grande variedade de habitats disponíveis, possibilitando uma alta diversidade microbiana. A distribuição espacial dos micro-organismos é influenciada por fatores locais e regionais. Os fatores locais são associados à estrutura do ambiente e os fatores regionais, a limitação na dispersão dos micro-organismos que compõem as comunidades e eventos históricos que eventualmente podem modificar o ambiente. Eventos como a liberação de hidrocarbonetos das camadas mais profundas do sedimento para superfície
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36

Li, Yuting. "Investigating sediment size distributions and size-specific Sm-Nd isotopes as paleoceanographic proxy in the North Atlantic Ocean : reconstructing past deep-sea current speeds since Last Glacial Maximum." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/273776.

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To explore whether the dispersion of sediments in the North Atlantic can be related to modern and past Atlantic Meridional Overturning Circulation (AMOC) flow speed, particle size distributions (weight%, Sortable Silt mean grain size) and grain-size separated (0–4, 4–10, 10–20, 20–30, 30–40 and 40–63 μm) Sm-Nd isotopes and trace element concentrations are measured on 12 cores along the flow-path of Western Boundary Undercurrent and in the central North Atlantic since the Last glacial Maximum (LGM). North Atlantic is a useful place to explore how size-specific sediment provenance is related to
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37

Joussain, Ronan. "Histoire de l’érosion de l’Himalaya durant le dernier cycle climatique : approches sédimentologiques, minéralogiques et géochimiques des sédiments de la partie proximale de l’éventail sous-marin profond du Bengale." Thesis, Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLS433.

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L’objectif de cette étude est de reconstruire le régime de l’érosion des chaînes himalayennes, et de relier ces paramètres aux variations climatiques globales et à l’intensité de la mousson. Dans ce travail, Les sédiments de 3 carottes prélevées dans la baie du Bengale pendant la mission MONOPOL ont fait l’objet d’analyses minéralogiques (XRD et granulométrie) et géochimiques (majeurs, traces, la composition isotopique du Nd et du Sr). La mise en âge des carottes, est basée sur les enregistrements de δ¹⁸O de foraminifères planctoniques (G. ruber), et des datations au ¹⁴C (AMS). Ces 3 enregistr
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38

Arason, Pórdur. "Paleomagnetic inclination shallowing in deep-sea sediments." Thesis, 1991. http://hdl.handle.net/1957/29238.

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In this thesis anomalous downcore shallowing of paleomagnetic inclinations is interpreted to be caused by sediment compaction. Thus, compaction-induced inclination shallowing may influence tectonic reconstructions that are based on inclinations from deep-sea sediment cores. Progressive downcore shallowing of the remanent inclination was observed in a 120-m section of Plio- Pleistocene sediments at Deep Sea Drilling Project (DSDP) site 578 in the northwest Pacific. Near the top of the section the average inclination corresponds to the expected geocentric axial dipole value of 53° but shallows d
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39

"Paleoceanography of the Agulhas Current and retroflection determined by radiogenic isotopes in deep-sea sediments." COLUMBIA UNIVERSITY, 2008. http://pqdtopen.proquest.com/#viewpdf?dispub=3299357.

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Dwan, Shufa F. "A seismic refraction study of the Monterey Deep Sea Fan and a comparison of velocity structures among fan subunits." Thesis, 1986. http://hdl.handle.net/1957/29229.

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A deep source-receiver seismic refraction experiment was conducted on the upper part of the Monterey Deep Sea Fan. The aim of this thesis is to construct the velocity structure of the upper Monterey Fan and to examine the lateral seismic velocity variations among the upper, middle and lower fan subunits. Using primary waves and whispering gallery phases (the multiply-reflected refraction waves), the sediment velocity structure was modeled by the tau-zeta travel time inversion process. The changes in velocity gradients with depth of the upper Monterey Fan are morphologically similar to that fou
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41

Schauer, Regina [Verfasser]. "Diversity and function of microbial communities in sediments from different deep-sea habitats / vorgelegt von Regina Schauer." 2010. http://d-nb.info/1012929752/34.

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42

Dias, Ágata. "Geochemistry of deep-sea hydrothermal sediments from the Saldanha and Lucky Strik hydrothermal fields : (Mid-Aatlantic Rridge)." Doctoral thesis, 2009. http://hdl.handle.net/10451/1618.

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Tese de doutoramento, Geologia (Cristalografia e Mineralogia), Universidade de Lisboa, Faculdade de Ciências, 2009<br>Disponível no documento<br>Fundação para a Ciência e a Tecnologia (SFRH/BD/8896/2002 FSE/POCI 2010), U.I. CREMINER LA/ISR (POSC 518) and projects AMAR (Praxis XXI/2/2.1/MAR/1748/95) and SEAHMA (POCTI/MAR/15281/1999).
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43

Muller, Anne. "Deep-sea sediment core and coral reconstructions of the Late Quaternary paleoceanography of the eastern Indian Ocean." Phd thesis, 2002. http://hdl.handle.net/1885/151776.

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44

Chih-HuaChen and 陳志華. "Evolution of Deep Water Circulation in the South China Sea in the Last 30Ma:REEs and Nd-Hf isotopic compositions of Fe-Mn oxide coating in sediments." Thesis, 2010. http://ndltd.ncl.edu.tw/handle/70889828405702073594.

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碩士<br>國立成功大學<br>地球科學系碩博士班<br>98<br>This study aims to develop a robust sequential leaching technique for extracting Nd isotopes in the Fe-Mn oxide coatings. The sediment core, ODP site 1148, was selected to study the seawater isotopic evolution of the South China Sea (SCS) since 30 Ma years ago. The distribution of the PAAS-normalized REE pattern from the extracted fraction displays a clear MREE-enriched pattern, which reveals a strong authigenic Fe-Mn oxyhydroxides in marine sediments. Tracings of the source and variability of deep-water mass shifting can be achieved by applying the Nd and Hf
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45

Tsai, Ching-Hui, and 蔡慶輝. "Study of crustal structures and deep-sea sediment waves in the northern South China Sea." Thesis, 2007. http://ndltd.ncl.edu.tw/handle/90322780924963176476.

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博士<br>國立中央大學<br>地球物理研究所<br>95<br>There are two main topics presented in this thesis. First is to use reflection seismic data and gravity modeling to study the crustal structures in the northern continental margin of the South China Sea (SCS). Another topic is to use high resolution seismic and chirp sonar data to study deep-sea sedimemt waves in the north and south sides of downstream of the Formosa Canyon. Additionally, we present the foundamatal procedures of data collecting and processing of the multi-beam bathymetry data and show a preliminary result of new bathymetry map off southwest Tai
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46

Marassi, Rithielli Rodrigues. "Ecotoxicology of deep-sea environments: effects of suspended sediment under hyperbaric conditions." Master's thesis, 2021. https://hdl.handle.net/10216/136720.

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47

Liu, De-Yu, and 劉得鈺. "Structural Features and Sediment Distribution in the South China Sea Deep Sea Basin from Seismic Reflection Profile Analysis." Thesis, 2015. http://ndltd.ncl.edu.tw/handle/69987581417293055255.

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48

Lahajnar, Niko [Verfasser]. "Organic matter degradation in the deep sea : results from sediment trap studies and surface sediment sampling / vorgelegt von Niko Lahajnar." 2006. http://d-nb.info/981696511/34.

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49

Weng, Chieh-Yin, and 翁杰愔. "Isolation and Characterization of Methanoculleus and Methanosarcina from deep sea marine sediment offshore SW of Taiwan." Thesis, 2014. http://ndltd.ncl.edu.tw/handle/73013147295837212131.

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碩士<br>國立中興大學<br>生命科學系所<br>102<br>Taiwan is situated on the boundary separating the Eurasian plate to the west from the Philippine Sea Plate to the east. There were complex landforms from SW of Taiwan, such as ridges, mud volcanos, cold seeps and gas hydrate bearing regions. The isotopic data from Prof. Tsan-Yao Yang’s lab was suggested that most of the methane produced in Taiwan methane hydrate potential area is biogenic origin. To explore the methanogens at methane seeps or hydrate habitats, sediment samples obtained from piston core at Tainan Ridge, Good Weather Ridge, 96 Mud Volcano and Def
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Wen, Jen-Chih, and 温閏植. "The Inversion for Sediment Acoustic Parameters Using Surface Sound Source with Biot Theory in Deep Sea Area." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/33165108411068775077.

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碩士<br>國立中山大學<br>海下科技暨應用海洋物理研究所<br>102<br>Due to locating in subtropical zone with high-speed sea water sound velocity, Taiwan Navy fleet’s sonar energy can not avoid to contact with sea bottom for ASW purpose. Seabed topography affects the reflection of sound rays, and sediment acoustic parameters affect reflected energy as well. To predict sonar performance, sediment acoustic parameters, such as sound speed, effective density and attenuation, are necessaries. Estimating these parameters is the main purpose of this thesis. Base on two-ship acoustic experiment, use NTURAY to calculate sound ra
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