Relevant bibliographies by topics / BigH3

Academic literature on the topic 'BigH3'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "BigH3"

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Page, Lionel, Bozena Polok, Mauro Bustamante, and Daniel F. Schorderet. "Bigh3 Is Upregulated in Regenerating Zebrafish Fin." Zebrafish 10, no. 1 (March 2013): 36–42. http://dx.doi.org/10.1089/zeb.2012.0759.

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Ellies, Pierre, Gilles Renard, Sophie Valleix, Pierre Yves Boelle, and Paul Dighiero. "Clinical outcome of eight BIGH3-linked corneal dystrophies." Ophthalmology 109, no. 4 (April 2002): 793–97. http://dx.doi.org/10.1016/s0161-6420(01)01025-9.

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Allaman-Pillet, Nathalie, Anne Oberson, Mauro Bustamante, Andrea Tasinato, Edith Hummler, and Daniel F. Schorderet. "Tgfbi/Bigh3 silencing activates ERK in mouse retina." Experimental Eye Research 140 (November 2015): 159–70. http://dx.doi.org/10.1016/j.exer.2015.09.004.

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Schmitt-Bernard, C. F., Y. Pouliquen, and A. Argilès. "Protéine BIGH3 : mutation du codon 124 et amylose cornéenne." Journal Français d'Ophtalmologie 27, no. 5 (May 2004): 510–22. http://dx.doi.org/10.1016/s0181-5512(04)96173-6.

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Shah, A. A., G. Wen, K. S. C. Chao, and T. K. Hei. "The Role of BigH3 in Mesothelioma Pathogenesis and Radiosensitivity." International Journal of Radiation Oncology*Biology*Physics 78, no. 3 (November 2010): S627. http://dx.doi.org/10.1016/j.ijrobp.2010.07.1459.

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Mondragon, Albert A., Brandi S. Betts-Obregon, Robert J. Moritz, Kalpana Parvathaneni, Mary M. Navarro, Hong Seok Kim, Chi Fung Lee, Richard G. LeBaron, Reto Asmis, and Andrew T. Tsin. "BIGH3 protein and macrophages in retinal endothelial cell apoptosis." Apoptosis 20, no. 1 (November 7, 2014): 29–37. http://dx.doi.org/10.1007/s10495-014-1052-6.

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Thoma, Brian S., Robert J. Moritz, Fatemeh Rezapoor, Chandler T. Sargent, Clyde F. Phelix, and Richard G. LeBaron. "BIGH3: A Negative Regulator of Human Osteosarcoma Large Multicellular Spheroids." International Journal of Clinical Medicine 07, no. 11 (2016): 771–91. http://dx.doi.org/10.4236/ijcm.2016.711084.

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Kocak-Altintas, Ayse Gül, Inci Kocak-Midillioglu, A. Nurten Akarsu, and Sunay Duman. "BIGH3 Gene Analysis in the Differential Diagnosis of Corneal Dystrophies." Cornea 20, no. 1 (January 2001): 64–68. http://dx.doi.org/10.1097/00003226-200101000-00013.

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Klamer, Sofieke E., Carlijn GM Kuijk, Peter L. Hordijk, C. Ellen van der Schoot, Marieke von Lindern, Paula B. van Hennik, and Carlijn Voermans. "BIGH3 modulates adhesion and migration of hematopoietic stem and progenitor cells." Cell Adhesion & Migration 7, no. 5 (September 25, 2013): 434–49. http://dx.doi.org/10.4161/cam.26596.

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Ellies, Pierre, Riad Antoine Bejjani, Jean Louis Bourges, Pierre Yves Boelle, Gilles Renard, and Paul Dighiero. "Phototherapeutic keratectomy for BIGH3-linked corneal dystrophy recurring after penetrating keratoplasty." Ophthalmology 110, no. 6 (June 2003): 1119–25. http://dx.doi.org/10.1016/s0161-6420(03)00229-x.

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Dissertations / Theses on the topic "BigH3"

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Dighiero, Paul. "Genetique moleculaire des dystrophies de cornee liees au gene bigh3 : implications pronostiques et therapeutiques." Paris 6, 2001. http://www.theses.fr/2001PA066289.

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Les dystrophies corneennes hereditaires sont un vaste groupe de maladies, le plus souvent de transmission autosomique dominante, dont la definition reposait naguere uniquement sur des donnees cliniques et histologiques. La decouverte du gene bigh3 (ou tgfi) et de ses mutations ont permis d'expliquer la plupart des dystrophies corneennes frequentes. Ce gene code pour une proteine, ig-h3, de 683 acides amines, ubiquitaire et dont le role exact demeure encore inconnu. ig-h3 a pu etre detectee dans la plupart des tissus composes d'une matrice extra-cellulaire (comme la cornee). L'opacification corneenne observee au cours des mutations du gene bigh3, s'explique par l'accumulation de depots de proteine ig-h3 mutee. Notre travail sur les dystrophies corneennes hereditaires liees a ce gene a permis : 1) de decrire les caracteristiques cliniques, histologiques et ultrastructurales de 3 nouvelles mutations du gene bigh3 (r124l, r124l+del125-126 et a546t) responsables de nouveaux phenotypes de dystrophies de cornee. 2) de comparer, par l'etude histologique et ultrastructurale, les differents depots corneens associes a huit mutations differentes du gene bigh3 et d'expliquer les formes anciennement atypiques. 3) d'etablir que chaque mutation presentait une evolution clinique propre quant a l'age de necessite d'un traitement chirurgical et de proposer un traitement adapte a chaque mutation. 4) de decrire les caracteristiques des depots corneens rencontres au cours des dystrophies liees au gene bigh3, grace a la microscopie confocale. En conclusion, la meilleure connaissance des caracteristiques cliniques et histologiques des dystrophies corneennes liees au gene bigh3, grace notamment a la genetique moleculaire, permet deja d'ameliorer la prise en charge chirurgicale des patients, ainsi que d'envisager la therapie genique par transfection des cellules souches corneennes.
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Oberbeckmann, Sonja [Verfasser]. "Vibrio spp. in the German Bight / Sonja Oberbeckmann." Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2012. http://d-nb.info/1035216922/34.

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Cossa, Obadias J. "Modelling the oceanic circulation in the Delagoa Bight." Doctoral thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/27911.

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The ROMS is used to investigate the oceanic circulation in the Delagoa Bight region, near the southwestern end of the Mozambique Channel. The model is initially configured at a horizontal resolution of 1/10° (9.9km) over the domain 30.1-43°E,22.13-30.8° S. Subsequent configurations nested an inner grid of resolution 1/30° (3.3km) over the region 32.43-36.43°E,24.09-27.71°S Several sensitivity experiments were performed with and without the inner grid or with or without tidal forcing. Using only the outer coarse resolution grid, the first experiment (DELAGI) does not include tidal forcing whereas tides are included in the second (DELAG-II) experiment. DELAG-III and DELAG-IV both use the inner higher resolution grid but exclude and include tidal forcing respectively. The model was evaluated against observations, namely the WOA, Pathfinder SST and AVISO SSH. The results showed that ROMS adequately resolves the oceanic features in the region, namely the pathways of the anticyclonic eddies from the northern Mozambique Channel and from Madagascar, and the instances when the DBLE is present or absent. The model is also able to reproduce the main water masses and their sources in the region. Water masses found in the centre of the Bight enter through the northeastern sector, either by intrusion of pulses or instabilities of the southwards flowing current. When the DBLE is well established, upwelling is likely to contribute to the water masses in the lower layers. The transport of water towards the Bight from the east was found to be less than that from the north. The model also succeeds in representing the thermocline structure of the DBLE but it fails to capture the local salinity maximum. When tidal forcing is included, the speed of the flow close to the coast increases. The model also revealed the influence of the Inhambane Cyclone on the Delagoa Bight as well as on the region to its south. This cyclone, which is generated in the flow near Inhambane, is similar to Natal Pulses which occur in the Agulhas Current. An eddy detecting and tracking system was used with both the model outputs and VISO SSH to determine the statistics of the DBLE, namely its dimensions, amplitudes and life-times. A maximum radius of 59.52 km, life span of 126 days and an amplitude of 27.27 cm were found. It was also demonstrated that this feature is generated northeast of the Bight. When the inner grid was included in the simulations, anticyclonic features were generated within the Bight with a maximum diameter of 85.4 km and life span of 12 day. These anticyclonic features dominate the circulation when the DBLE is absent (less than 30 percent of the total period of the simulation). The possibility of several cyclonic cores existing simultaneously in the Bight was also demonstrated. Two cores were found with life spans of more than 12 days. When the number of cores is greater than two, they tend to be short lived. Analysis of energy conversion rates showed that the generation of both the DBLE and the Inhambane cyclones is mainly by barotropic instabilities, although in both regions of their generation, weak baroclinic instabilities were also found.
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D'Agostino, Anthony F. "Three dimensional acoustic effects in the Middle Atlantic Bight." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1996. http://handle.dtic.mil/100.2/ADA314805.

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Thesis (M.S. in Meteorology and Physical Oceanography) Naval Postgraduate School, June 1996.
Thesis advisor(s):Ching-Sang Chiu, Kevin B. Smith. "June 1996. Bibliography: p. 39-40. Also available online.
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Linder, Christopher Anthony. "A climatology of the Middle Atlantic Bight shelfbreak front." Thesis, Monterey, California. Naval Postgraduate School, 1996. http://hdl.handle.net/10945/8093.

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Description of the shelfbreak front in the Middle Atlantic Bight is hampered by the extreme variability of the front. In order to gain more insight into the mean frontal structure and associated baroclinic jet, historical data is used to produce two dimensional climatological fields of temperature and salinity for the region south of Nantucket shoals. Associated cross-shelf fields of density, geostrophic velocity, relative vorticity, and shallow water potential vorticity have also been computed. Historical data from a quality- controlled database (HydroBase) in the region 69-72 deg W, 39.5-41 deg N is included. Cross-shelf sections are obtained by averaging the data in nine depth bins with an average cross-shelf spacing of 10 km but an increased resolution of 4 km near the shelfbreak. The vertical averaging interval was 10 m over the shelf and upper slope waters, increasing to 50 m in the deep slope waters. The data were averaged in bimonthly periods to study seasonal trends. For inter- regional comparison, similar analyses were performed for the south flank of Georges Bank and the shelf off New Jersey. The climatological temperature and salinity are consistent with previous descriptions of the frontal hydrography. Most importantly, features such as the cold pool, the upper slope pycnostad, and the frontal boundary are well resolved when compared with synoptic sections. The temperature contrast across the front varies seasonally between 2-6 deg C near the surface and at depths of 45-65 m. The salinity contrast is 1.5-2 PSS, with little seasonal variation. The resulting cross-frontal near surface density gradients are strongest during the winter and weakest during the summer, when the seasonal thermocline is established
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Linder, Christopher A. (Christopher Anthony) 1972. "A climatology of the Middle Atlantic Bight shelfbreak front." Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/41009.

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Sharples, Alexander Gabriel William david. "Tectono-stratigraphic evolution of the Cenozoic Great Australian Bight." Thesis, University of Manchester, 2014. https://www.research.manchester.ac.uk/portal/en/theses/tectonostratigraphic-evolution-of-the-cenozoic-great-australian-bight(7025cc3d-1faa-4b0d-91d3-1bb514ee9237).html.

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The Great Australian Bight (GAB) is an extensive W-E striking continental margin basin that drifted northwards during the Cenozoic following rifting and separation from Antarctica in the mid/late Cretaceous. Seafloor spreading accelerated in the mid-Eocene and was associated with local volcanism. The mid-Eocene succession of the GAB is conspicuously mounded and separates a dominantly siliciclastic succession below from a fully marine carbonate succession above. The mounded succession was penecontemporaneous with major changes in global climate, oceanographic conditions and tectonic re-organization in the region, and thus may hold important clues as to the palaeo-environmental changes associated with these changes. The mid Eocene has so far only been described locally or in passing, usually by studies focused on either the siliciclastics below or the carbonates above. It was therefore chosen as a major focus point for the research project reported herein. Exploration activity in the GAB has been limited despite the presence of a working petroleum system and large target structures, but industry interest has increased over the past few years leading to 3D seismic surveys being acquired in the GAB. The focus for exploration is the Cretaceous succession beneath the relatively thin Cenozoic cover, which however, is still important in terms of shallow hazards and as overburden to the anticipated productive sections. As is often the case, the new 3D seismic data shows many overburden features in great detail and thus affords new insights to be gained that improve our understanding of the post-rift evolution of the marginThis thesis expands upon and reinterprets a pre-existing sequence framework in the Cenozoic GAB based from ODP Leg 182 results. A vast database of 2D and 3D seismic surveys has been integrated with exploration wells and borehole data and several surfaces have been calibrated to borehole and well constraints, then mapped to the maximum lateral extent across the available dataset. Surface mapping provided new insight into sequence deposition and palaeoenvironmental settings. Structure maps and thickness maps highlight key depocentre locations and trends over the Cenozoic GAB as well as stacked mass debris aprons. The newly discovered sequences raise new questions regarding trigger mechanisms in a-seismic areas and feed into industry geohazard perception models. The base surface of the Cenozoic framework hosts a plethora of mounded features across shelf and basinal section. All mounds within the dataset have been mapped. A set a bryozoan reef mounds have been interpreted lying parallel to the margin as linear complexes over 500 km. They coincide with the underlying siliciclastic delta clinoform breakpoints and provide insight into the changing palaeoenvironment at the 43 Ma mark, cessation of siliciclastics and regional marine transgression. Further mound mapping aided by 3D attribute extractions along the base Cenozoic unconformity led to the interpretation of a series of enigmatic igneous-based mounded features. The discoveries have been included in a comparative study, comparing all mounded features (igneous or carbonate) and contrasting their individual characteristics of geometry, seismic facies, dimension in order to understand mound origin and emplacement. A new grouping of mounds in the GAB has been established, the origin and emplacement mechanisms of which contribute to the global knowledge base.
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Ruiz, Alfredo. "Web-based tidal toolbox of astronomic tidal data for the Atlantic Intracoastal Waterway, esturaries sic] and continental shelf of the South Atlantic Bight." Master's thesis, University of Central Florida, 2011. http://digital.library.ucf.edu/cdm/ref/collection/ETD/id/5021.

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A high-resolution astronomic tidal model has been developed that includes detailed inshore regions of the Atlantic Intracoastal Waterway and associated estuaries along the South Atlantic Bight. The unique nature of the model's development ensures that the tidal hydrodynamic interaction between the shelf and estuaries is fully described. Harmonic analysis of the model output results in a database of tidal information that extends from a semi-circular arc (radius ~750 km) enclosing the South Atlantic Bight from the North Carolina coast to the Florida Keys, onto the continental shelf and into the full estuarine system. The need for tidal boundary conditions (elevation and velocity) for driving inland waterway models has motivated the development of a software application to extract results from the tidal database which is the basis of this thesis. In this tidal toolbox, the astronomic tidal constituents can be resynthesized for any open water point in the domain over any interval of time in the past, present, or future. The application extracts model results interpolated to a user's exact geographical points of interest, desired time interval, and tidal constituents. Comparison plots of the model results versus historical data are published on the website at 89 tidal gauging stations. All of the aforementioned features work within a zoom-able geospatial interface for enhanced user interaction. In order to make tidal elevation and velocity data available, a web service serves the data to users over the internet. The tidal database of 497,847 nodes and 927,165 elements has been preprocessed and indexed to enable timely access from a typical modern web server. The preprocessing and web services required are detailed in this thesis, as well as the reproducibility of the Tidal Toolbox for new domains.
ID: 029808889; System requirements: World Wide Web browser and PDF reader.; Mode of access: World Wide Web.; Thesis (M.S.)--University of Central Florida, 2011.; Includes bibliographical references (p. 182-184).
M.S.
Masters
Civil, Environmental and Construction Engineering
Engineering and Computer Science
Civil Engineering
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Kaemmerer, Glen E. "Simulation of acoustic multipath arrival structure in the Middle Atlantic Bight." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1995. http://handle.dtic.mil/100.2/ADA300804.

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Thesis (M.S. in Applied Physics) Naval Postgraduate School, June 1995.
"June 1995." Thesis advisor(s): James H. Miller, Ching-Sang Chiu, Kevin B. Smith. Bibliography: p. 63-66. Also available online.
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Hollebone, Amanda L. "An Invasive Crab in the South Atlantic Bight: Friend or Foe?" Diss., Connect to this title online, 2006. http://etd.gatech.edu/theses/available/etd-04092006-121221/.

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Thesis (Ph. D.)--Georgia Institute of Technology, 2006.
Title from PDF t.p. (viewed on Apr. 12, 2007). Streelman, J. Todd, Committee Member ; Miller, Margaret, Committee Member ; Weissburg, Marc, Committee Member ; Snell, Terry, Committee Member ; Hay, Mark, Committee Chair. Includes bibliographical references (p. 104-113).
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Books on the topic "BigH3"

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McFarlane, Lucy Fitzpatrick. Tickle & bight. St. John's NL, Canada: James Lane Publishing, 2010.

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Nilkant. Ek bigha khet. Allahabad: Sahitya Bhandar, 1992.

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The battle of Heligoland Bight. Bloomington: Indiana University Press, 2006.

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McCutchan, Philip. Halfhyde at the Bight of Benin. Ithaca, N.Y: McBooks Press, 2004.

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Huh, Chih-An. Historical contamination in the Southern California Bight. Silver Spring, Md: Coastal Monitoring and Bioeffects Assessment Division, Office of Ocean Resources Conservation and Assessment, National Ocean Service, National Oceanic and Atmospheric Administration, U.S. Dept. of Commerce, 1998.

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Eppley, R. W., ed. Plankton Dynamics of the Southern California Bight. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ln015.

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Silent storytellers of Totem Bight State Historical Park. Anchorage: Alaska Geographic Association, 2009.

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Cantillo, Adriana Y. MESA New York Bight Project water column chemistry data: Cruises #6-12 of the NOAA ship Ferrel, April-November 1974. Miami, Fla: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Atlantic Oceanographic and Meterological Laboratory, 1997.

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D'Agostino, Anthony F. Three dimensional acoustic effects in the Middle Atlantic Bight. Monterey, Calif: Naval Postgraduate School, 1996.

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Linder, Christopher Anthony. A climatology of the Middle Atlantic Bight shelfbreak front. Springfield, Va: Available from National Technical Information Service, 1996.

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Book chapters on the topic "BigH3"

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Dethlefsen, V. "German Bight." In Pollution of the North Sea, 425–40. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-73709-1_23.

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Hirota, E., K. Kuchitsu, T. Steimle, J. Vogt, and N. Vogt. "40 BiH3 Bismuthine." In Molecules Containing No Carbon Atoms and Molecules Containing One or Two Carbon Atoms, 70. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-540-70614-4_41.

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Demaison, J. "15 BiH3 Bismuthine." In Symmetric Top Molecules, 51–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-47532-3_17.

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Hayes, Miles O. "The Georgia Bight Barrier System." In Geology of Holocene Barrier Island Systems, 233–304. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-78360-9_7.

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Nichols, C. Reid, Gary Zarillo, and Christopher F. D’Elia. "Mid Atlantic Bight and Chesapeake Bay." In Tomorrow's Coasts: Complex and Impermanent, 241–59. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-75453-6_15.

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Carlucci, A. F., R. W. Eppley, and J. R. Beers. "Introduction to the Southern California Bight." In Plankton Dynamics of the Southern California Bight, 1–12. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ln015p0001.

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Jackson, G. A. "Physical oceanography of the Southern California Bight." In Plankton Dynamics of the Southern California Bight, 13–52. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ln015p0013.

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Eppley, R. W., and O. Holm-Hansen. "Primary production in the Southern California Bight." In Plankton Dynamics of the Southern California Bight, 176–215. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ln015p00176.

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Brockmann, U. H., and K. Eberlein. "River Input of Nutrients into the German Bight." In The Role of Freshwater Outflow in Coastal Marine Ecosystems, 231–40. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-70886-2_15.

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Heyde, I. "Aerogravity Survey of the German Bight (North Sea)." In Gravity, Geoid and Earth Observation, 37–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-10634-7_6.

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Conference papers on the topic "BigH3"

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RezaPoor, F., R. Moritz, CF Phelix, and RG LeBaron. "Abstract P6-02-03: TGF-b1-inducible protein BIGH3 (transforming growth factor beta-induced gene human clone 3): A new mechanism inducing breast cancer cell apoptosis." In Abstracts: Thirty-Sixth Annual CTRC-AACR San Antonio Breast Cancer Symposium - Dec 10-14, 2013; San Antonio, TX. American Association for Cancer Research, 2013. http://dx.doi.org/10.1158/0008-5472.sabcs13-p6-02-03.

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Suszkowski, D., and E. Santoro. "Marine Monitoring in the New York Bight." In OCEANS '86. IEEE, 1986. http://dx.doi.org/10.1109/oceans.1986.1160432.

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Nawaz, Manica, and John Chamberlain. "HOLOCENE CONCRETIONS FROM THE NEW YORK BIGHT." In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-375065.

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Nawaz, Manica, and John Chamberlain. "AGE AND ORIGIN OF NY BIGHT CONCRETIONS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379852.

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Wilkens, Jort, Nils Asp, Klaus Ricklefs, and Roberto Mayerle. "Medium-Scale Morphodynamic Modelling in the Meldorf Bight." In World Water and Environmental Resources Congress 2001. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40569(2001)268.

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Dibke, C., M. Fischer, and B. M. Scholz-Böttcher. "Microplastic Abundance and Distribution in German Bight Surface Waters." In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902846.

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Howden, Stephan D., and Amy Kern. "Circulation on the continental shelf within the Mississippi Bight." In SPIE Defense, Security, and Sensing, edited by Weilin W. Hou and Robert A. Arnone. SPIE, 2013. http://dx.doi.org/10.1117/12.2018079.

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Amirshahi, S., C. Winter, and E. Kwoll. "Characteristics of instantaneous turbulent events in southern German Bight." In The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742: CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-32.

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Bulpitt, W. S., S. W. Stewart, M. H. Hunt, and S. V. Shelton. "Feasibility of Offshore Wind Power in the South Atlantic Bight." In Offshore Technology Conference. Offshore Technology Conference, 2006. http://dx.doi.org/10.4043/18351-ms.

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Woodhams, C. A., E. Heshmati, and A. C. Ruskin. "Great Australian Bight: New Offshore Frontiers, Challenges and Potential Solutions." In Offshore Technology Conference. Offshore Technology Conference, 2017. http://dx.doi.org/10.4043/27529-ms.

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Reports on the topic "BigH3"

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Scholz, Florian. Sedimentary fluxes of trace metals, radioisotopes and greenhouse gases in the southwestern Baltic Sea Cruise No. AL543, 23.08.2020 – 28.08.2020, Kiel – Kiel - SEDITRACE. GEOMAR Helmholtz Centre for Ocean Research Kiel, November 2020. http://dx.doi.org/10.3289/cr_al543.

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Abstract:
R/V Alkor Cruise AL543 was planned as a six-day cruise with a program of water column and sediment sampling in Kiel Bight and the western Baltic Sea. Due to restrictions related to the Covid-19 pandemic, the original plan had to be changed and the cruise was realized as six oneday cruises with sampling in Kiel Bight exclusively. The first day was dedicated to water column and sediment sampling for radionuclide analyses at Boknis Eck and Mittelgrund in Eckernförde Bay. On the remaining five days, water column, bottom water, sediment and pore water samples were collected at eleven stations covering different types of seafloor environment (grain size, redox conditions) in western Kiel Bight. The data and samples obtained on cruise AL543 will be used to investigate (i) the sedimentary cycling of bio-essential metals (e.g., nickel, zinc, and their isotopes) as a function of variable redox conditions, (ii) the impact of submarine groundwater discharge and diffusive benthic fluxes on the distribution of radium and radon as well as greenhouse gases (methane and nitrous oxide) in the water column, and (iii) to characterize and quantify the impact of coastal erosion on sedimentary iron, phosphorus and rare earth element cycling in Kiel Bight.
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Barans, Charles A. South Atlantic Bight Synoptic Offshore Observational Network. Fort Belvoir, VA: Defense Technical Information Center, August 2002. http://dx.doi.org/10.21236/ada405456.

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Barans, Charlie. South Atlantic Bight Synoptic Offshore Observational Network. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630543.

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Miller, James H. Middle Atlantic Bight Field Study: SUS Component. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada634891.

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Glenn, Scott, Dale B. Haidvogel, and Hernan Arango. Sediment Transport Modeling in the New York Bight. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada628036.

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Lapota, David. Seasonal Planktonic Bioluminescence in the Southern California Bight. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada629292.

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Gawarkiewicz, Glen. Quantifying Ocean Thermal Variability in the Middle Atlantic Bight. Fort Belvoir, VA: Defense Technical Information Center, December 2000. http://dx.doi.org/10.21236/ada389938.

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Kean, B. F., and D. T. W. Evans. Geology and Mineralization of the Lushs Bight Group Springdale Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132255.

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Gawarkiewicz, Glen, James Lynch, and Albert Plueddemann. Tidal Analysis Near the Shelfbreak in the Middle Atlantic Bight. Fort Belvoir, VA: Defense Technical Information Center, June 2001. http://dx.doi.org/10.21236/ada389617.

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Smith, Kevin B. 3D Propagation and Geoacoustic Inversion Studies in the Mid-Atlantic Bight. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630677.

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