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Relevant bibliographies by topics / Paleoshorelines

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Academic literature on the topic 'Paleoshorelines'

Author: Grafiati

Published: 4 June 2021

Last updated: 6 February 2022

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Journal articles on the topic "Paleoshorelines"

1

Laws, Alexander W., Jillian M. Maloney, Shannon Klotsko, Amy E. Gusick, Todd J. Braje, and David Ball. "Submerged paleoshoreline mapping using high-resolution Chirp sub-bottom data, Northern Channel Islands platform, California, USA." Quaternary Research 93 (October 18, 2019): 1–22. http://dx.doi.org/10.1017/qua.2019.34.

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AbstractHigh-resolution Chirp sub-bottom data were obtained offshore from the Northern Channel Islands (NCI), California, to image submerged paleoshorelines and assess local uplift rates. Although modern bathymetry is often used for modeling paleoshorelines, Chirp data image paleoshorelines buried beneath sediment that obscures their seafloor expression. The NCI were a unified landmass during the last glacial maximum (LGM; ~20 ka), when eustatic sea level was ~120 m lower than present. We identified seven paleoshorelines, ranging from ~28 to 104 m in depth, across this now-submerged LGM platform. Paleoshoreline depths were compared to local sea-level curves to estimate ages, which suggest that some were reoccupied over multiple sea-level cycles. Additionally, previous studies determined conflicting uplift rates for the NCI, ranging from 0.16 to 1.5 m/ka. Our results suggest that a rate on the lower end of this range better fits the observed submerged paleoshorelines. Using the uplift rate of ~0.16 m/ka, we estimate that paleoshorelines formed during Marine Oxygen Isotope Stage 3, the LGM, and the Younger Dryas stade are preserved on the NCI platform. These results help clarify uplift rates for the NCI and illustrate the importance of sub-bottom data for mapping submerged paleoshorelines.

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Mancini, Marco, Elisabetta D'Anastasio, Mario Barbieri, and Paolo Marco De Martini. "Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy)." Quaternary Research 67, no. 3 (2007): 487–501. http://dx.doi.org/10.1016/j.yqres.2007.01.005.

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AbstractThe eastern border of the Middle Valley of the Tiber River is characterized by several Plio-Pleistocene paleoshorelines, which extend for about 100 km along the western margin of the Central Apennines (Italy). We studied these paleoshorelines by the means of geological and paleontological analyses and new 87Sr/86Sr isotope analyses. The youngest and uppermost paleoshorelines have been detected and mapped through detailed geologic and stratigraphic surveys, which led to the recognition of nearshore deposits, cliff breccias, alignments of Lithophaga borings, fossil abrasion notches and wave-cut platforms. The altitude of these paleoshorelines decreases almost regularly in the NNW–SSE direction from 480 to 220 m a.s.l. Measurements of the 87Sr/86Sr isotope ratio have been conducted on corals and mollusks collected from sediments outcropping close to the paleoshorelines. The isotopic dating results indicate numerical values that range between 0.70907 and 0.70910 all over the 100-km outcrop. These results, together with biostratigraphic data, constrain the age of the youngest paleoshorelines to 1.65–1.50 Ma. These paleoshorelines are thus considered almost isochronous, giving an estimated uplift rate of 0.34–0.17±0.03 mm/a moving from NNW to SSE. Shape, length and continuity of the 100-km-long observed movements indicate that the studied paleoshorelines are an important marker of the Quaternary uplift of the Central Apennines.

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Sanchez, Gabriel M., Jon M. Erlandson, and Nicholas Tripcevich. "Quantifying the association of chipped stone crescents with wetlands and paleoshorelines of western North America." North American Archaeologist 38, no. 2 (2016): 107–37. http://dx.doi.org/10.1177/0197693116681928.

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In America’s Far West, chipped stone crescents dating between approximately 12,000 to 8000 cal BP are often found associated with Western Stemmed Tradition points. Crescent function is debated, but scholars have suggested that they are closely associated with wetland habitats, an association that has never been systematically investigated. Using a geographic information system-based Euclidean distance analysis, we compared a sample of 100 geolocated crescent-bearing sites in Washington, Oregon, Idaho, Nevada, Utah, and California with reconstructed paleoshorelines. We confirmed a strong association of crescents with wetlands—94 of the 100 sites and approximately 99% of crescents themselves were located within 10 km of reconstructed paleoshorelines. Our results provide quantitative and region-wide support for a strong association of crescents with terminal Pleistocene and early Holocene wetland habitats. The diversity of aquatic habitats crescents are associated with, along with their morphology, suggests an association with faunal rather than plant resources, possibly birds of the Pacific Flyway.

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Mouslopoulou, Vasiliki, John Begg, Andrew Nicol, Onno Oncken, and Christine Prior. "Formation of Late Quaternary paleoshorelines in Crete, Eastern Mediterranean." Earth and Planetary Science Letters 431 (December 2015): 294–307. http://dx.doi.org/10.1016/j.epsl.2015.09.007.

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Dickinson, William R. "Control of paleoshorelines by trench forebulge uplift, Loyalty Islands." Quaternary Research 80, no. 1 (2013): 125–37. http://dx.doi.org/10.1016/j.yqres.2013.04.007.

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Unlike most tropical Pacific islands, which lie along island arcs or hotspot chains, the Loyalty Islands between New Caledonia and Vanuatu owe their existence and morphology to the uplift of pre-existing atolls on the flexural forebulge of the New Hebrides Trench. The configuration and topography of each island is a function of distance from the crest of the uplifted forebulge. Both Maré and Lifou are fully emergent paleoatolls upon which ancient barrier reefs form highstanding annular ridges that enclose interior plateaus representing paleolagoon floors, whereas the partially emergent Ouveapaleoatoll rim flanks a drowned remnant lagoon. Emergent paleoshoreline features exposed by island uplift include paleoreef flats constructed as ancient fringing reefs built to past low tide levels and emergent tidal notches incised at past high tide levels. Present paleoshoreline elevations record uplift rates of the islands since last-interglacial and mid-Holocene highstands in global and regional sea levels, respectively, and paleoreef stratigraphy reflects net Quaternary island emergence. The empirical uplift rates vary in harmony with theoretical uplift rates inferred from the different positions of the islands in transit across the trench forebulge at the trench subduction rate. The Loyalty Islands provide a case study of island environments controlled primarily by neotectonics.

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Lee, J., Sheng-Hua Li, and J. C. Aitchison. "OSL dating of paleoshorelines at Lagkor Tso, western Tibet." Quaternary Geochronology 4, no. 4 (2009): 335–43. http://dx.doi.org/10.1016/j.quageo.2009.02.003.

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Ruiz, Javier, Alberto G. Fairén, James M. Dohm, and Rosa Tejero. "Thermal isostasy and deformation of possible paleoshorelines on Mars." Planetary and Space Science 52, no. 14 (2004): 1297–301. http://dx.doi.org/10.1016/j.pss.2004.06.003.

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Bouton, Anthony, Emmanuelle Vennin, Julien Boulle, et al. "Linking the distribution of microbial deposits from the Great Salt Lake (Utah, USA) to tectonic and climatic processes." Biogeosciences 13, no. 19 (2016): 5511–26. http://dx.doi.org/10.5194/bg-13-5511-2016.

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Abstract. The Great Salt Lake is a modern hypersaline lake, in which an extended modern and ancient microbial sedimentary system has developed. Detailed mapping based on aerial images and field observations can be used to identify non-random distribution patterns of microbial deposits, such as paleoshorelines associated with extensive polygons or fault-parallel alignments. Although it has been inferred that climatic changes controlling the lake level fluctuations explain the distribution of paleoshorelines and polygons, straight microbial deposit alignments may underline a normal fault system parallel to the Wasatch Front. This study is based on observations over a decimetre to kilometre spatial range, resulting in an integrated conceptual model for the controls on the distribution of the microbial deposits. The morphology, size and distribution of these deposits result mainly from environmental changes (i.e. seasonal to long-term water level fluctuations, particular geomorphological heritage, fault-induced processes, groundwater seepage) and have the potential to bring further insights into the reconstruction of paleoenvironments and paleoclimatic changes through time. New radiocarbon ages obtained on each microbial macrofabric described in this study improve the chronological framework and question the lake level variations that are commonly assumed.

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van Andel, Tjeerd H. "Holocene book reviews : Paleoshorelines and prehistory: an investigation of methods." Holocene 3, no. 2 (1993): 188. http://dx.doi.org/10.1177/095968369300300213.

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Fedje, Daryl W., and Tina Christensen. "Modeling Paleoshorelines and Locating Early Holocene Coastal Sites in Haida Gwaii." American Antiquity 64, no. 4 (1999): 635–52. http://dx.doi.org/10.2307/2694209.

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AbstractThe integration of archaeology and paleoecology has allowed a fuller understanding of the history of southern Haida Gwaii and provided insights into the regional history of coastal occupation in northwestern North America. Of particular consequence is the history of sea-level fluctuations during the late-glacial and early Holocene. The modern shore holds only part of the history of coastal occupation. Much is flooded or hidden in the rainforest. In southern Haida Gwaii, shorelines dating from 13,000 to 9,500 B.P. are deeply drowned while those dating from 9,200 to 3,000 B.P. are stranded in the rainforest up to 15 meters above modern levels. Shorelines have been approximately coincident with the current position for only the last two to three millennia and for a century or two centered around 9,400 B.P. Modeling these paleoshorelines has led to discovery and investigation of a number of early Holocene archaeological sites.

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Dissertations / Theses on the topic "Paleoshorelines"

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Konfal, Stephanie Ann. "Analysis of Antarctic Crustal Motion Using Remote Sensing and GPS Data: Applications to Ice Mass Change Studies." The Ohio State University, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=osu1337813324.

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Dilworth, John R. "Analysis and Chronology of Glacial Lake Arkona in the Western Lake Erie Basin, USA." University of Toledo / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=toledo1501791567833752.

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Baitis, Elke Elise. "Patterns and paleoshorelines of White Sands Dune Field, New Mexico." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-05-3354.

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The dune field at White Sands, New Mexico, shows a well-defined pattern of dunes and interdune areas, as well as spatial variations in this pattern. The purpose of this research is to determine which measured pattern parameters are most consistent across the dune field and to determine the cause of depositional spatial variability. This was accomplished using an airborne LiDAR generated digital-elevation model (DEM) collected in June 2007 and covering 39 km² of the dune field. Properties of the dune field are defined by measurements from three dune populations: 1) 110 randomly selected dunes, 2) 247 dunes along transects oriented in the net transport direction, and 3) 171 dunes from three zones within the field where differences in pattern are visible. Measurements of eight common dune parameters show that the lowest coefficients of variation occur with dune orientation and crestline sinuosity, which largely define the field pattern. Cross-plotting of parameters shows generally poor correlations, which is thought to reflect variation around field-scale means that are comparable to other dune fields globally. Removing the dunes from the LiDAR DEM reveals a depositional substrate with breaks in slope interpreted as three paleoshorelines associated with Pleistocene Lake Otero. The paleoshorelines are antecedent boundary conditions that exert the primary control on spatial variability within the dune pattern.<br>text

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"Geomorphic and structural evolution of relay ramps during normal fault interaction and linkage." Tulane University, 2016.

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acase@tulane.edu<br>Geomorphic features such as fluvial channels and shorelines can act as tape recorders of accumulated tectonic deformation. Because these features can survive in a landscape for up to105 years, the deformation represents tectonic activity over timescales longer than earthquake cycles but shorter than geological timescales. Deformed landscape features can be used to understand the impact of changing tectonic rates on landscape evolution (given information on the tectonic processes involved). Conversely, we can take advantage of how a landscape is expected to evolve and utilize those deviations to explore details of tectonic processes that do not manifest over short timescales (i.e. single earthquakes). Fault slip rate is expected to increase within the overlapping region of two en echelon normal faults, but how increasing slip rate affects the landscape is poorly understood (as discussed in Chapter 1). Additionally, details of this tectonic process that occur over geomorphic timescales are not clearly understood. Chapter 2 of this dissertation explores the impact of fault slip rate increase on fluvial channels during normal fault interaction and linkage. Results of this work show that the landscape responds by increasing channel slope and decreasing channel width before fault segments link. Channel width only shows sustained decreases when a threshold channel slope of about 0.05 is exceeded. In Chapter 3 vertically deformed lacustrine shorelines are mapped along linked faults through the former overlap zones. These results show that despite the presence of linking structures between faults, portions of the former overlapping tips remain active post-linkage for 104 years. Chapter 4 investigates the effect of fault length, spacing, and overlap on the area of relay ramps that drains parallel to fault strike. Twenty-seven sites are examined and results show that for fault lengths below 15 km most of the relay ramp area drains parallel to fault strike, whereas fault lengths >15 km no particular drainage geometry is favored. Data on the overlap/spacing ratio are biased to <2 for faults above ~15 km length. This bias is an inherent characteristic because faults that define low overlap/spacing ratio relays do not link rapidly and are, therefore, preserved within the landscape along large mature fault systems. The results of this dissertation show that, while faults are mechanically interacting, relay ramps are dynamic features that have significant impacts on landscape evolution. Following complete linkage between segments, the relays do not behave as passive structures and can actively deform over significant (>104 years) timescales. Finally, the structural geometry of relay ramps impacts long-term morphodynamics and channel network topology, which directly influences basin sedimentary architecture in extensional basins.<br>1<br>Michael C. Hopkins

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Anderton, John Baye. "Paleoshoreline geoarchaeology in the northern Great Lakes an interdisciplinary approach to prehistoric coastal settlement /." 1995. http://catalog.hathitrust.org/api/volumes/oclc/33290009.html.

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Thesis (Ph. D.)--University of Wisconsin--Madison, 1995.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 158-168).

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Books on the topic "Paleoshorelines"

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Lewis, Johnson Lucille, and Stright Melanie, eds. Paleoshorelines and prehistory: An investigation of method. CRC Press, 1992.

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Johnson, Lucille Lewis. Paleoshorelines and Prehistory: An Investigation of Method (Telford Press). CRC, 1991.

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3

Nearshore Marine Paleoclimatic Regions, Increasing Zoogeograpic Provinciality, Molluscan Extinctions, and Paleoshorelines, California: Late Oligocene (27 ... Paper (Geological Society of America)). Geological Society of America, 2002.

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Hall, Clarence A. Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: late Oligocene (27 Ma) to late Pliocene (2.5 Ma). Geological Society of America, 2002. http://dx.doi.org/10.1130/spe357.

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Special Paper 357: Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: late Oligocene (27 Ma) to late Pliocene (2.5 Ma). Geological Society of America, 2002. http://dx.doi.org/10.1130/0-8137-2357-4.

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Dickinson, William R. Coastal Landforms on Islands of Pacific Oceania. Edited by Ethan E. Cochrane and Terry L. Hunt. Oxford University Press, 2014. http://dx.doi.org/10.1093/oxfordhb/9780199925070.013.023.

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The evolution of coastal landforms on tropical Pacific islands has been influenced jointly by changes in relative sea level and by shoreline sediment dynamics. During human occupation of Pacific Oceania, changes in sea level have reflected a monotonic hydro-isostatic drawdown in regional sea level following a mid-Holocene highstand in eustatic sea level, and varied patterns of tectonic uplift or subsidence affecting individual islands or island groups. Wave erosion has altered some bold coastlines, but the dominant trend of paleoshoreline evolution along lowland coasts has been the expansion of coastal plains by the accretion of successive beach ridges to island cores as regional sea level gradually fell. Anthropogenic impacts on island landscapes have influenced strandline sedimentation by enhancing sediment delivery to island coasts in response to inland deforestation.

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Book chapters on the topic "Paleoshorelines"

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Halligan, Jessi. "Lake Ontario Paleoshorelines and Submerged Prehistoric Site Potential in the Great Lakes." In When the Land Meets the Sea. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-8210-0_3.

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Erkeling, Gino, Giovanni Leone, and Ákos Kereszturi. "Paleoshoreline." In Encyclopedia of Planetary Landforms. Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4614-9213-9_248-1.

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Erkeling, Gino, Giovanni Leone, and Ákos Kereszturi. "Paleoshoreline." In Encyclopedia of Planetary Landforms. Springer New York, 2015. http://dx.doi.org/10.1007/978-1-4614-3134-3_248.

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Hall, Clarence A. "Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: Late Oligocene (27 Ma) to late Pliocene (2.5 Ma)." In Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: late Oligocene (27 Ma) to late Pliocene (2.5 Ma). Geological Society of America, 2002. http://dx.doi.org/10.1130/0-8137-2357-4.1.

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Conference papers on the topic "Paleoshorelines"

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Miller, D. E., Carlos Montejo, Jesus Eduardo Moreno, et al. "MID-CENOZOIC PALEOSHORELINES, WESTERN TEHACHAPI-EASTERN SAN EMIGDIO MTNS CA." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-362683.

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Wykel, C. Andrew, and William Richardson Doar. "GEOMORPHIC ANALYSIS OF PALEOSHORELINES IN HORRY COUNTY, SOUTH CAROLINA: 1967 VERSUS 2018." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-327644.

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Ameen, Fadhil, and P. Othman. "New paleoshorelines of the prolific Oligocene /Aquitanian sequence from zagros fold thrut belt.Kurdistan Region/N.Iraq." In First EAGE Workshop on Iraq - Hydrocarbon Exploration and Field Development. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143562.

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MCBRIDE, RANDOLPH A., MARK R. BYRNES, and LOUIS D. BRITSCH. "SUBSIDENCE-CORRECTED ELEVATIONS OF PALEOSHORELINES (CHENIER RIDGES) OF THE MISSISSIPPI RIVER CHENIER PLAIN, USA: IMPLICATIONS FOR FORCING MECHANISMS." In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0014.

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Thornton, Erik, and Kathleen M. Farrell. "SEDIMENTARY FACIES AND BOUNDING SURFACES ASSOCIATED WITH THE EARLY PLEISTOCENE SURRY PALEOSHORELINE COMPLEX, COASTAL PLAIN, NORTH CAROLINA." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290309.

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Riddick, Nicholas, Joseph I. Boyce, Vasıf Şahoğlu, Irfan Tuğcuc, and Yeşim Alkan. "PALEOSHORELINE RECONSTRUCTION AND UNDERWATER ARCHAEOLOGICAL POTENTIAL OF LIMAN TEPE: A LONG-OCCUPIED COASTAL PREHISTORIC SITE IN WESTERN TURKEY." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359279.

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Farrell, Kathleen M., and Katie L. Cummings. "A FIELD METHOD OF DEFINING AND MAPPING EARLY PLEISTOCENE SEQUENCES USING GEOPROBE CORES – SURRY PALEOSHORELINE COMPLEX, COASTAL PLAIN, NORTH CAROLINA." In 65th Annual Southeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016se-273470.

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Farrell, Kathleen M., and Erik Thornton. "REEXAMINATION OF SEVERAL EARLY (LOWER) PLEISTOCENE FORMATIONS IN THE CONTEXT OF SEQUENCE STRATIGRAPHY, SURRY PALEOSHORELINE COMPLEX, NORTH CAROLINA COASTAL PLAIN." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-326226.

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Farrell, Kathleen M., and Erik Thornton. "USING HIGH-RESOLUTION LIDAR FOR GEOMORPHIC AND STRATIGRAPHIC MAPPING OF THE COASTAL PLAIN AT A SCALE OF 1:8000, SURRY PALEOSHORELINE COMPLEX, NORTH CAROLINA." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-311996.

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Reports on the topic "Paleoshorelines"

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Tackman, G., and D. Currey. Paleoshoreline and lake gauge evidence for post-Lake Agassiz regional tilting in Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207527.

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