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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Continental margins. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (559 pages)
    Edition: 1st ed.
    ISBN: 9780470766361
    Series Statement: International Association of Sedimentologists Series ; v.25
    DDC: 551.3/53
    Language: English
    Note: Intro -- Preface -- Writing a Rosetta stone: insights into continental-margin sedimentary processes and strata -- CHARLES A. NITTROUER*, JAMES A. AUSTIN JR†, MICHAEL E. FIELD‡, JOSEPH H. KRAVITZ, JAMES P.M. SYVITSKI¶ and PATRICIA L. WIBERG** -- INTRODUCTION -- THE BOUNDARY CONDITIONS -- THE COMMON THREADS -- Eel River (California) continental margin -- New Jersey continental margin -- SEDIMENT DELIVERY -- General considerations -- Delivery of Eel margin sediment -- SEDIMENT ALTERATION -- General considerations -- Alteration of Eel margin sediment -- SEDIMENT DISPERSAL SYSTEM -- General considerations -- Eel margin sediment dispersal system -- SEABED FAILURE -- General considerations -- Eel margin failure -- GRAVITY FLOWS -- General considerations -- MARGIN MORPHOLOGY -- General considerations -- New Jersey margin morphology -- Eel margin morphology -- MARGIN STRATIGRAPHY -- General considerations -- New Jersey margin stratigraphy -- Eel margin stratigraphy -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- REFERENCES -- Sediment delivery to the seabed on continental margins -- PAUL S. HILL*, JASON M. FOX*, JOHN S. CROCKETT†, KRISTIAN J. CURRAN*, CARL T. FRIEDRICHS‡, W. ROCKWELL GEYER, TIMOTHY G. MILLIGAN¶, ANDREA S. OGSTON†, PERE PUIG**, MALCOLM E. SCULLY‡, PETER A. TRAYKOVSKI and ROBERT A. WHEATCROFT†† -- INTRODUCTION -- REVIEW OF PREVIOUS WORK -- Early conceptual models -- Sediment loss from discharge plumes -- Advective transport in river plumes -- Bottom-boundary-layer transport of flood sediment -- Summary of past research -- SEDIMENT DELIVERY TO THE EEL MARGIN -- Site description -- Observational programme -- Results -- Fate of missing sediment -- SUMMARY AND CONCLUSION -- Summary of STRATAFORM sediment delivery -- Questions for future research -- ACKNOWLEDGEMENTS -- NOMENCLATURE -- REFERENCES. , Post-depositional alteration and preservation of sedimentary strata -- ROBERT A. WHEATCROFT*, PATRICIA L. WIBERG†, CLARK R. ALEXANDER‡, SAMUEL J. BENTLEY, DAVID E. DRAKE¶, COURTNEY K. HARRIS** and ANDREA S. OGSTON†† -- INTRODUCTION AND SCOPE -- CONSOLIDATION -- Theoretical framework -- Observations -- PHYSICAL ALTERATION -- Fluid forcing -- Bed properties -- Deposition -- BIOLOGICAL ALTERATION -- Alteration of key dynamical bed properties -- Bioturbation -- Biogenic sedimentary structures -- PRESERVATION -- Controlling parameters -- Dissipation times -- The key role of episodic sedimentation -- SUMMARY -- ACKNOWLEDGEMENTS -- NOMENCLATURE -- REFERENCES -- Oceanic dispersal and accumulation of river sediment -- CHRISTOPHER K. SOMMERFIELD*, ANDREA S. OGSTON†, BETH L. MULLENBACH‡, DAVID E. DRAKE, CLARK R. ALEXANDER¶, CHARLES A. NITTROUER†, JEFFRY C. BORGELD**, ROBERT A. WHEATCROFT†† and ELANA L. LEITHOLD‡‡ -- INTRODUCTION -- Margin sediment dispersal systems: a Holocene perspective -- Research background -- QUANTIFYING SEDIMENTARY PROCESSES -- Suspended-sediment transport -- Sediment deposition and accumulation -- THE NORTHERN CALIFORNIA MARGIN -- Previous work and insight -- SEDIMENT PRODUCTION AND COASTAL DELIVERY -- Tectonics and sediment yield -- Hydroclimatology and recorded streamflow -- Floods, land use and sediment delivery -- Coastal ocean circulation -- SEDIMENT TRANSPORT AND ACCUMULATION -- Mechanisms of sediment transport -- Dynamic trapping mechanisms -- Static trapping mechanisms -- SEDIMENTATION PATTERNS AND RATES -- Sedimentary event deposition -- Centennial to millennial accumulation -- Latest Holocene sedimentary record -- Accumulation rates and stratigraphic completeness -- SEDIMENT BUDGETS OF DISPERSAL SYSTEMS -- Development of sediment budgets -- Eel margin sediment budget -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- NOMENCLATURE. , REFERENCES -- Submarine mass movements on continental margins -- HOMA J. LEE*, JACQUES LOCAT†, PRISCILLA DESGAGNÉS†, JEFFREY D. PARSONS‡, BRIAN G. McADOO, DANIEL L. ORANGE¶, PERE PUIG**, FLORENCE L. WONG*, PETER DARTNELL* and ERIC BOULANGER† -- INTRODUCTION -- HISTORIC DEVELOPMENT OF UNDERSTANDING -- CLASSIFICATION -- ENVIRONMENTS -- Fjords -- Active river deltas on the continental shelf -- Submarine canyon-fan systems -- The open continental slope -- STATISTICS OF SUBMARINE LANDSLIDES -- MECHANICS OF SLOPE FAILURE -- Driving stress -- Resisting stress (strength) -- Slope stability analysis -- PORE-WATER PRESSURE -- SEDIMENT MOBILIZATION AND STRENGTH LOSS -- TRIGGERS -- Sediment accumulation -- Erosion -- Earthquakes -- Volcanoes -- Waves -- Gas and gas hydrates -- Groundwater seepage -- Diapirism -- Human activity -- CONTRIBUTIONS TO SUBMARINE LANDSLIDE RESEARCH FROM THE STRATAFORM PROJECT -- 'Humboldt Slide' controversy -- Liquefaction failures in Eel Canyon -- Gas charging and pore pressures -- Development of shear strength and rheology in marine sediment -- Submarine landslide geomorphology -- Regional mapping of landslide susceptibility -- SUMMARY -- Overall occurrence and triggers -- Controversies -- Importance of the liquidity index -- Pore pressures and the development of anomalously weak sediment -- Development of anomalously high strength -- Slope stability analysis and regional assessment of landslide susceptibility -- An important contribution -- ACKNOWLEDGEMENTS -- NOMENCLATURE -- REFERENCES -- The mechanics of marine sediment gravity flows -- JEFFREY D. PARSONS*, CARL T. FRIEDRICHS†, PETER A. TRAYKOVSKI‡, DAVID MOHRIG, JASIM IMRAN¶, JAMES P.M. SYVITSKI**, GARY PARKER††, PERE PUIG‡‡, JAMES L. BUTTLES and MARCELO H. GARCÍA†† -- INTRODUCTION -- TURBIDITY CURRENTS -- Basic mechanics -- Frontal dynamics -- Turbidity-current fans. , Channelization and channel processes -- Observations of turbidity currents -- DEBRIS FLOWS -- Basic mechanics -- Hydroplaning -- Advances in analytical and numerical solutions -- Observations of submarine debris flows -- WAVE-SUPPORTED SEDIMENT GRAVITY FLOWS -- Wave-boundary-layer mechanics -- Wave-supported sediment gravity flows and the role of buoyancy -- Vertical distribution of momentum and sediment concentration -- Observations of wave-supported sediment gravity flows -- ORIGIN AND TRANSFORMATION OF SEDIMENT GRAVITY FLOWS -- Failure-induced formation -- Wave/tide-induced formation -- Direct formation from river loading -- Linkages between phenomena -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- NOMENCLATURE -- REFERENCES -- Seascape evolution on clastic continental shelves and slopes -- LINCOLN F. PRATSON*, CHARLES A. NITTROUER†, PATRICIA L. WIBERG‡, MICHAEL S. STECKLER, JOHN B. SWENSON¶, DAVID A. CACCHIONE**, JEFFERY A. KARSON*, A. BRADLEY MURRAY*, MATTHEW A. WOLINSKY*, THOMAS P. GERBER*, BETH L. MULLENBACH††, GLENN A. SPINELLI‡‡, CRAIG -- INTRODUCTION -- From bathymetry to seascape evolution -- Scope of paper -- BACKGROUND -- Physiographical definitions -- Historical interest in and importance of the continental shelf and slope -- PROCESSES GOVERNING SHELF WIDTH AND SLOPE RELIEF -- Plate tectonics and the stair-step shape of continental margins -- First-order effects of thermal subsidence and tectonic uplift -- Second-order effects of isostasy, compaction and faulting -- Added effects of faulting -- PROCESSES THAT FORM THE SHELF PROFILE -- Rivers, deltas and growth of the coastal plain -- Bedload deposition, sediment plumes and clinoforms -- The impacts of waves and currents on the shelf and shoreface profile -- Subaqueous deltas and wave-supported sediment gravity flows -- Independent movements of the shoreline and shelf break. , Shelf evolution during sea-level change -- PROCESSES THAT ACT TO LIMIT THE SLOPE OF THE CONTINENTAL SLOPE -- Seafloor failure and submarine groundwater flow -- Bottom shear from internal waves -- Turbidity-current erosion and deposition -- PROCESSES THAT CREATE SUBMARINE CANYONS AND SLOPE GULLIES -- Turbidity currents versus seafloor failure in forming submarine canyons -- Turbidity currents versus seafloor failure in forming slope gullies -- FUTURE RESEARCH -- ACKNOWLEDGEMENTS -- REFERENCES -- The long-term stratigraphic record on continental margins -- GREGORY S. MOUNTAIN*, ROBERT L. BURGER†, HEIKE DELIUS‡, CRAIG S. FULTHORPE, JAMIE A. AUSTIN, DAVID S. GOLDBERG¶, MICHAEL S. STECKLER¶, CECILIA M. McHUGH**, KENNETH G. MILLER*, DONALD H. MONTEVERDE*, DANIEL L. ORANGE†† and LINCOLN F. PRATSON‡‡ -- INTRODUCTION -- Distinguishing time-scales -- The importance of the long-term record -- Long-term geochronology: dating continental-margin records -- ANALYSING THE LONG-TERM RECORD -- Basin-wide surfaces and long-term processes -- Tools for accessing the long-term record -- THE EEL RIVER BASIN -- Tectonism - a major control of sediment distribution and preservation -- Offshore stratigraphy - local variations of governing processes -- Stratigraphic modelling -- THE NEW JERSEY MARGIN -- Cenozoic sedimentation on a passive margin -- Pleistocene sequences -- The last eustatic cycle and its preserved record -- New Jersey submarine canyons -- Stratigraphic modelling -- SUMMARY -- The long-term record: its challenges and rewards -- The Eel River Basin: difficulties in recognizing eustatic control -- The New Jersey margin: eustatic imprint, with complications -- The long-term record - where next? -- ACKNOWLEDGEMENTS -- REFERENCES -- Prediction of margin stratigraphy. , JAMES P.M. SYVITSKI*, LINCOLN F. PRATSON†, PATRICIA L. WIBERG‡, MICHAEL S. STECKLER, MARCELO H. GARCÍA¶, W. ROCKWELL GEYER**, COURTNEY K. HARRIS††, ERIC W.H. HUTTON*, JASIM IMRAN‡‡, HOMA J. LEE, MARK D. MOREHEAD¶¶ and GARY PARKER***.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 28 (1981), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The ridge and swale topography of the Middle Atlantic Bight is best developed on the Delaware-Maryland inner shelf. Here sand ridges can be seen in all stages of formation. Several aspects of the ridge field are pertinent to the problem of ridge genesis. The first is ridge morphology. There is a systematic morphologic change from shoreface ridges through nearshore ridges to offshore ridges, which reflects the changing hydraulic regime. As successively more seaward ridges are examined, maximum side slope decreases, the ratio of maximum seaward slope to maximum landward slope decreases, and the cross-sectional area increases. These changes in ridge morphology with depth and distance from shore appear to be equivalent to the morphologic changes experienced by a single ridge during the course of the Holocene transgression.A second aspect is the change in bottom sediment characteristics that accompanies these large-scale morphologic changes. Megaripples, sand waves and mud lenses appear in the troughs between nearshore and offshore ridges. These changes indicate that the storm flows which maintain ridges are less frequently experienced in the deeper sector, and that the role of high-frequency wave surge becomes less important relative to the role of the mean flow component in shaping the sea-floor.A third aspect is the systematic relationship of grain size to topography. Grain size is 90° out of phase with topography, so that the coarsest sand lies between the axis of the landward trough and the ridge crest, while the finest sand lies between the ridge crest and the axis of the seaward trough. This relationship is characteristic of large-scale bedforms.Finally, flow was measured and transport calculated on the same ridge during a one-month period (November 1976). Threshold was exceeded only during storm events. Mean transport was southerly and a little seaward with respect to both the ridge crest and the shoreline. These flow measurements are in conformity with the pattern of smaller bedforms. A 43-year time series of bathymetric change for this ridge reveals a systematic pattern of landward flank erosion, seaward flank deposition, and seaward crest migration.Sand ridges are considered the consequence of constructive feedback between an initial topography and the resulting distribution of bottom shear stress. The relationship between grain size and topography supports this model, but does not account directly for the oblique angle of the ridge with respect to the coastline. This feature may be due to a more rapid alongshore migration rate of the inshore edge of the ridge than the offshore edge, and the relationship between this migration rate, and the rate of shoreface retreat.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 226 (1970), S. 836-837 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Thin sections of the rocks reveal the presence of individual euhedral cubic pyrite crystals as well as the relative abundance of the framework grains. Calcareous grains incorporated into the rocks seem to have undergone selective dissolution during cementation. Outer surfaces of the two ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 2 (1982), S. 135-141 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In 1980, a large earthquake caused extensive sediment failure on the shallow continental shelf off the Klamath River in northern California. Side-scan sonography was used to complement detailed geophysical profiling in identifying specific features and resolving modes of failure. The features include a nearly flat failure terrace mantled with sand boils, collapse craters and sediment flows, and bounded on the seaward side by a meandering continuous toe ridge. Seaward of the terrace lies a compression zone delineated by small pressure ridges. Our findings indicate a temporal progression of failure from lique-faction of shallow subsurface sand to lateral spread of intact blocks to sediment collapse and flow.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 1 (1981), S. 33-37 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Several aspects of the Maryland ridge field are pertinent to the problem of ridge genesis in response to Holocene sea-level rise. There is a systematic morphologic change fromshoreface ridges throughnearshore ridges tooffshore ridges, which reflects the changing hydraulic regime. Grain size is 90° out of phase with topography, so that the coarsest sand lies between the axis of each trough and the adjacent seaward ridge crest, while the finest sand lies between each ridge crest and the axis of the adjacent seaward trough. Finally, analysis over a 43-year period on an outer ridge reveals a systematic pattern of landward flank erosion, seaward flank deposition, and seaward crest migration. These relationships support a model which explains the ridges as consequences of the up-current shift of maximum bottom shear stress with respect to the crests of initial bottom irregularities. The oblique orientation of the ridges with respect to the beach may be at least partly due to the more rapid migration rate of the ridges’ inshore ends.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2014-04-03
    Description: Author(s): Kyle J. Peterson, Thomas J. Awe, Edmund P. Yu, Daniel B. Sinars, Ella S. Field, Michael E. Cuneo, Mark C. Herrmann, Mark Savage, Diana Schroen, Kurt Tomlinson, and Charles Nakhleh Recent experiments on Sandia’s Z facility have confirmed simulation predictions of dramatically reduced instability growth in solid metallic rods when thick dielectric coatings are used to mitigate density perturbations arising from an electrothermal instability. These results provide further eviden... [Phys. Rev. Lett. 112, 135002] Published Wed Apr 02, 2014
    Keywords: Plasma and Beam Physics
    Print ISSN: 0031-9007
    Electronic ISSN: 1079-7114
    Topics: Physics
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  • 7
    Publication Date: 2022-05-25
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Marine Pollution Bulletin 52 (2006): 1034-1047, doi:10.1016/j.marpolbul.2006.01.008.
    Description: Sediment traps were used to evaluate the frequency, cause, and relative intensity of sediment mobility/resuspension along the fringing coral reef off southern Molokai (February 2000–May 2002). Two storms with high rainfall, floods, and exceptionally high waves resulted in sediment collection rates 〉 1000 times higher than during non-storm periods, primarily because of sediment resuspension by waves. Based on quantity and composition of trapped sediment, floods recharged the reef flat with land-derived sediment, but had a low potential for burying coral on the fore reef when accompanied by high waves. The trapped sediments have low concentrations of anthropogenic metals. The magnetic properties of trapped sediment may provide information about the sources of land-derived sediment reaching the fore reef. The high trapping rate and low sediment cover indicate that coral surfaces on the fore reef are exposed to transient resuspended sediment, and that the traps do not measure net sediment accumulation on the reef surface.
    Keywords: Coral reef ; Sediment ; Sediment traps ; Chemical composition ; Magnetic properties ; Molokai
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 8
    Publication Date: 2022-05-26
    Description: © The Authors, 2010. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Coral Reefs 30 (2011): 23-38, doi:10.1007/s00338-010-0705-3.
    Description: Sediment traps are commonly used as standard tools for monitoring “sedimentation” in coral reef environments. In much of the literature where sediment traps were used to measure the effects of “sedimentation” on corals, it is clear from deployment descriptions and interpretations of the resulting data that information derived from sediment traps has frequently been misinterpreted or misapplied. Despite their widespread use in this setting, sediment traps do not provide quantitative information about “sedimentation” on coral surfaces. Traps can provide useful information about the relative magnitude of sediment dynamics if trap deployment standards are used. This conclusion is based first on a brief review of the state of knowledge of sediment trap dynamics, which has primarily focused on traps deployed high above the seabed in relatively deep water, followed by our understanding of near-bed sediment dynamics in shallow-water environments that characterize coral reefs. This overview is followed by the first synthesis of near-bed sediment trap data collected with concurrent hydrodynamic information in coral reef environments. This collective information is utilized to develop nine protocols for using sediment traps in coral reef environments, which focus on trap parameters that researchers can control such as trap height (H), trap mouth diameter (D), the height of the trap mouth above the substrate (z o ), and the spacing between traps. The hydrodynamic behavior of sediment traps and the limitations of data derived from these traps should be forefront when interpreting sediment trap data to infer sediment transport processes in coral reef environments.
    Keywords: Sediment trap ; Coral reefs ; Sedimentation ; Waves ; Currents ; Shear stress
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 9
    Publication Date: 2022-05-26
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Continental Shelf Research 24 (2004): 1397-1419, doi:10.1016/j.csr.2004.02.010.
    Description: The fringing coral reef off the south coast of Molokai, Hawaii is currently being studied as part of a US Geological Survey (USGS) multi-disciplinary project that focuses on geologic and oceanographic processes that affect coral reef systems. For this investigation, four instrument packages were deployed across the fringing coral reef during the summer of 2001 to understand the processes governing fine-grained terrestrial sediment suspension on the shallow reef flat (h=1 m) and its advection across the reef crest and onto the deeper fore reef. The time–series measurements suggest the following conceptual model of water and fine-grained sediment transport across the reef: Relatively cool, clear water flows up onto the reef flat during flooding tides. At high tide, more deep-water wave energy is able to propagate onto the reef flat and larger Trade wind-driven waves can develop on the reef flat, thereby increasing sediment suspension. Trade wind-driven surface currents and wave breaking at the reef crest cause setup of water on the reef flat, further increasing the water depth and enhancing the development of depth-limited waves and sediment suspension. As the tide ebbs, the water and associated suspended sediment on the reef flat drains off the reef flat and is advected offshore and to the west by Trade wind- and tidally- driven currents. Observations on the fore reef show relatively high turbidity throughout the water column during the ebb tide. It therefore appears that high suspended sediment concentrations on the deeper fore reef, where active coral growth is at a maximum, are dynamically linked to processes on the muddy, shallow reef flat.
    Keywords: Coral reefs ; Waves ; Tides ; Suspended sediment ; Sediment flux ; Cross-shore transport
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 10
    Publication Date: 2022-05-26
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Marine Geology 264 (2009): 140-151, doi:10.1016/j.margeo.2009.05.002.
    Description: Oceanographic measurements and sediment samples were collected during the summer of 2006 as part of a multi-year study of coastal circulation and the fate of terrigenous sediment on coral reefs in Hanalei Bay, Kauai. The goal of this study was to better understand sediment dynamics in a coral reef-lined embayment where winds, ocean surface waves, and river floods are important processes. During a summer period that was marked by two wave events and one river flood, we documented significant differences in sediment trap collection rates and the composition, grain size, and magnitude of sediment transported in the bay. Sediment trap collection rates were well correlated with combined wave-current near-bed shear stresses during the non-flood periods but were not correlated during the flood. The flood's delivery of fine-grained sediment to the bay initially caused high turbidity and sediment collection rates off the river mouth but the plume dispersed relatively quickly. Over the next month, the flood deposit was reworked by mild waves and currents and the fine-grained terrestrial sediment was advected around the bay and collected in sediment traps away from the river mouth, long after the turbid surface plume was gone. The reworked flood deposits, due to their longer duration of influence and proximity to the seabed, appear to pose a greater long-term impact to benthic coral reef communities than the flood plumes themselves. The results presented here display how spatial and temporal differences in hydrodynamic processes, which result from variations in reef morphology and orientation, cause substantial variations in the deposition, residence time, resuspension, and advection of both reef-derived and fluvial sediment over relatively short spatial scales in a coral reef embayment.
    Keywords: Coral reefs ; Winds ; Waves ; Currents ; Sediment traps ; Sedimentation ; USA ; Hawaii ; Kauai
    Repository Name: Woods Hole Open Access Server
    Type: Article
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