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Tesi sul tema "Paleoecology - Quaternary"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 30 gennaio 2023

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1

Sawada, Michael Charles. "Late quaternary paleoclimates and biogeography of North America." Thesis, University of Ottawa (Canada), 2001. http://hdl.handle.net/10393/9031.

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Pollen, spores, and dinoflagellate cysts are used with the modern analog technique (MAT) to provide paleoclimate reconstructions for terrestrial and marine environments in northeastern North America. Multivariate analysis of marine and nearby terrestrial pollen sequences from Hudson Bay, Labrador and the St. Lawrence, differentiate tundra, boreal and deciduous forest assemblages in time and space. These three regions had differing climate histories with respect to deglaciation and air mass boundaries. Prior to 6000 14C yr BP, cooler temperatures reconstructed along the Labrador margins agree w

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2

Lacourse, Terri. "Late Quaternary vegetation history of Sulphur Lake, southwest Yukon Territory, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0005/MQ36711.pdf.

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3

Simpson, Emily. "Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia." Digital Commons @ East Tennessee State University, 2019. https://dc.etsu.edu/etd/3590.

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Land-use, feeding habits, and response to seasonality by Quaternary megaherbivores in Saltville, Virginia, is poorly understood. Stable isotope analyses of serially sampled Bootherium and Equus enamel from Saltville were used to explore seasonally calibrated (δ18O) patterns in megaherbivore diet (δ13C) and land-use (87Sr/86Sr). Overall, this dataset suggests an open forest with relatively constant temperatures year round that were similar to modern conditions. Neither Bootherium or Equus individuals spent a significant amount of time at higher elevations in the nearby Blue Ridge geologic provi

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4

Herring, Erin Mauryeen. "Late Quaternary and Holocene paleoecology of interior mesic forests of northern Idaho." Thesis, University of Oregon, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3644438.

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<p> The mesic forests distributed within the Rocky Mountains of northern Idaho are unique because many species contained within the forest are separated from their main distribution along the Pacific Northwest coast. It remains unclear whether most species within the inland disjunction survived the glacial periods of the Pleistocene, or whether they were more recently dispersed from coastal populations. To see if the dominant tree taxa of the mesic forests today could have persisted in a refugium south of the large ice sheets, four sediment cores were used to reconstruct the vegetation and cli

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5

Bergolc, Melanie L. "A Paleoenvironmental Analysis Using Fossil Insects in Late Quaternary Deposits in Indiana and Ohio." Bowling Green State University / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1092940677.

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6

Hu, Feng Sheng. "An ecosystem approach to the study of late-Quaternary environmental change in southwestern Alaska /." Thesis, Connect to this title online; UW restricted, 1994. http://hdl.handle.net/1773/5577.

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7

Herring, Erin. "Late Quaternary and Holocene Paleoecology of Interior Mesic Forests of Northern Idaho." Thesis, University of Oregon, 2014. http://hdl.handle.net/1794/18509.

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The mesic forests distributed within the Rocky Mountains of northern Idaho are unique because many species contained within the forest are separated from their main distribution along the Pacific Northwest coast. It remains unclear whether most species within the inland disjunction survived the glacial periods of the Pleistocene, or whether they were more recently dispersed from coastal populations. To see if the dominant tree taxa of the mesic forests today could have persisted in a refugium south of the large ice sheets, four sediment cores were used to reconstruct the vegetation and climate

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8

Woolfenden, Wallace Bird 1941. "Late Quaternary vegetation history of the southern Owens Valley region, Inyo County, California." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/282184.

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This study analyzes the pollen, spores, and algae in the upper 90 m section of a mostly continuous, well dated, 323 m core (OL-92) from Owens Lake, southeastern California. The entire core has produced a paleoclimatic record for the past ∼800 ka. The 90 m interval dates from ∼9 ka to ∼151 ka beginning with the penultimate glaciation and ending during the termination of the last glaciation. The record shows high amplitude fluctuations in the abundances of pine, juniper, saltbush, sagebrush, chenopods/amaranths, and Ambrosia-type pollen. High percentages of juniper pollen with low percentages of

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9

Anshari, Gusti Zakaria. "Late quaternary vegetation and environments in the Lake Sentarum Wildlife Reserve, West Kalimantan, Indonesia." Monash University, School of Geography and Environmental Science, 2000. http://arrow.monash.edu.au/hdl/1959.1/9252.

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10

Sugden, Jean Mary. "Late quaternary palaeoecology of the central and marginal uplands of the Karoo, South Africa." Doctoral thesis, University of Cape Town, 1990. http://hdl.handle.net/11427/18278.

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Pollen analysis of organic sediments from vleis in upland areas of the Central and marginal Karoo has provided a vegetation history spanning the late Quaternary in the Winterberg, Sneeuberg, Nuweveldberg and Cederberg Mountains. Fossil pollen studies indicate moist conditions at the beginning of the Holocene, followed by a drier period. The second half of the Holocene (4 600 BP) is characterised by moister conditions, becoming drier towards the present and resulting in a decline in grasslands and an increase in Karoo-bushes. In the western Cape, the late Pleistocene (15 000 to 10 000 BP) was c

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11

Quillen, Amanda Kay. "Diatom-Based Paleolimnological Reconstruction of Quaternary Environments in a Florida Sinkhole Lake." FIU Digital Commons, 2009. http://digitalcommons.fiu.edu/etd/211.

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Despite lake sensitivity to climate change, few Florida paleolimnological studies have focused on changes in hydrology. Evidence from Florida vegetation histories raise questions about long-term hydrologic history of Florida lakes, and a 25-year limnological dataset revealed recent climate-driven effects on Lake Annie. The objectives of this research are (1) to use modern diatom assemblages to develop methods for reconstruction of climatic and anthropogenic change (2) to reconstruct both long-term and recent histories of Lake Annie using diatom microfossils. Paleoenvironmental reconstruction m

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12

Holmes, Jonathan Anthony. "Pliocene and Quaternary environmental change in Kashmir, north-west Himalaya." Thesis, University of Oxford, 1989. http://ora.ox.ac.uk/objects/uuid:e9bb6cf8-93a8-4471-9c55-7ed84044dc3c.

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Late Cainozoic environmental changes in Kashmir (33°30' to 34°30' N: 74°10' to 75°30' E) have been reconstructed using a range of techniques. The sedimentary record in Kashmir consists of a thick (>1000m) basin-fill sequence known as the Karewa group, together with glacial and related sediments in the surrounding mountain flanks. The Karewa sediments are fluviolacustrine in origin and comprise alternations of conglomerates, sands and clayey silts. Work on the lower Karewa formation, which has previously been dated palaeomagnetically to between 4 and 0.4 MaBP, involved the semi- quantitative an

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13

Dilley, Thomas Edward 1959. "Late Quaternary loess stratigraphy, soils, and environments of the Shaw Creek Flats Paleoindian sites, Tanana Valley, Alaska." Diss., The University of Arizona, 1998. http://hdl.handle.net/10150/282635.

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The late Quaternary stratigraphy of three Paleoindian archaeological sites, located on the edge of Shaw Creek Flats in the middle Tanana Valley, Alaska, consist of up to 2 meters of calcareous eolian sand, loess, and buried paleosols. Two Paleoindian occupations at the Broken Mammoth, Swan Point, and Mead sites date from 11,800 to 11,000 yr B.P. and from 10,800 to 9500 yr B.P. Well-preserved faunal remains, worked mammoth ivory, stone and organic tools, and at Swan Point, the early occurrence of microblades dating to 11,700 yr B.P., are associated with buried paleosols at the base of the loess

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14

Bergolc, Melanie. "A paleoenvironmental analysis using fossil insects in late Quaternary deposits in Indiana and Ohio." Connect to this title online, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=bgsu1092940677.

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15

Muiruri, Veronica Mwihaki. "Late Quaternary diatom and palynomorph stratigraphies and palaeoenvironments of the Koora Graben and Lake Magadi Basin, Kenya Rift Valley." HKBU Institutional Repository, 2017. https://repository.hkbu.edu.hk/etd_oa/461.

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Two sets of cores were recovered from the southern Kenya Rift (Koora and Magadi basins) through the Hominid Sites and Paleolakes Drilling Project and the Olorgesailie Drilling Project. These contain a detailed environmental Quaternary history with records of up to ~1 million years. This period correlates with much of the Olorgesailie Formation record of 1.2 Ma in the Olorgesailie Basin. The Magadi cores reached trachyte at ~ 194 and 133 m with this project focussed on the longer core, MAG14-2A, which includes limestone, zeolitic, laminated and massive clay and silt, massive mud, chert, trona,

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16

Cañellas, Boltà Núria. "Dinàmica de la vegetació en relació amb els canvis climàtics, els processos geològics i l'impacte humà a l'illa de Pasqua des del Glacial tardà. Estudi paleoecològic dels sediments del llac Rano Raraku." Doctoral thesis, Universitat de Barcelona, 2014. http://hdl.handle.net/10803/145926.

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Aquesta tesi doctoral es centra en la paleoecologia de l’Illa de Pasqua (Rapa Nui) (27ºS 109ºW). El present treball ha caracteritzat la vegetació a la conca del llac i la seva dinàmica com a resposta als canvis ambientals durant els darrers 34000 anys a partir d’indicadors ambientals (macrorestes vegetals, diatomees, registre palinològic, geoquímic i fàcies sedimentari) analitzats en sediments de testimonis de sondeig del llac Raraku. Els resultats han evidenciat variacions significatives en la composició de la vegetació en relació a canvis climàtics a llarg termini, modificacions de la morfol

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17

Gause, Austin. "Paleoenvironmental Reconstruction of Quaternary Saltville, Virginia, using Ostracode Autecology." Digital Commons @ East Tennessee State University, 2020. https://dc.etsu.edu/etd/3783.

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The Saltville valley in southwestern Virginia is home to Quaternary localities containing paleontological and archaeological remains. Historically the valley has been mined for salt and the small lakes, ponds and springs along the valley floor have a brackish signature. A preliminary report on the site’s ostracode fauna suggested that the site’s water was not always saline. This study analyzed modern and Quaternary ostracodes to understand the valley’s hydrologic and chemical evolution. Sediments contained primarily freshwater species, including the environmentally sensitive Candona crogmanian

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18

Yu, Zicheng. "Late Quaternary paleoecology of the southern Niagara Escarpment, Ontario, Canada, a multiple proxy investigation of vegetation and climate history." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq28098.pdf.

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19

Paixão, Jesus da Silva. "Contribuição à paleoecologia da Amazônia Meridional na planície de inundação do Rio Teles Pires, do norte do Estado do Mato Grosso." Universidade Federal de São Carlos, 2010. https://repositorio.ufscar.br/handle/ufscar/1673.

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Made available in DSpace on 2016-06-02T19:29:24Z (GMT). No. of bitstreams: 1 3085.pdf: 11800699 bytes, checksum: 71c066e8e0a2f17d9129aaf2bec7145c (MD5) Previous issue date: 2010-04-24<br>Records of isotopic and elemental carbon and nitrogen and pollen in lake sediments and soils have been used for studies of Quaternary paleoecology worldwide, including in the Amazon at specific sites, such as the region of Carajas, Lake Pata and Region Porto Velho in Rondonia state making it necessary to register in the central southern region. We collected two cores in the Lagoa Jabuti site and a core on th

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20

Anderson, Rodney Scott. "LATE-QUATERNARY ENVIRONMENTS OF THE SIERRA NEVADA, CALIFORNIA." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/184205.

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The pollen, plant macrofossil and aquatic fossil stratigraphies from a transect of sites in the Sierra Nevada, California, were examined to deduce paleoenvironmental change since the late-Wisconsinan. Fossil pollen samples were compared to modern pollen samples from both sides of the Sierra Nevada crest. Modern samples corresponded largely to modern vegetation units, validating the use of pollen for this purpose in mountainous environments. Vegetation change during the Holocene was largely contemporaneous on both sides of the crest at elevations where lake cores and meadow sections were analys

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21

Westaway, Kira E. "Reconstructing the Quaternary landscape evolution and climate history of western Flores an environmental and chronological context for an archaeological site /." Access electronically, 2006. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20070117.170105/index.html.

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22

Gossen, Candace Lynn. "Deforestation, Drought and Humans: New Discoveries of the Late Quaternary Paleoenvironment of Rapa Nui (Easter Island)." PDXScholar, 2011. https://pdxscholar.library.pdx.edu/open_access_etds/782.

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The mystery of the trees of Rapa Nui (Easter Island) is a complex problem within a dynamic ecosystem. With new physical cores from the volcanic crater lake Rano Kao, this dissertation uncovers a detailed 15,000 year ecological history of Easter Island and its climatic variability. New radiocarbon dating methods establish a more precise chronology which shows that the island before human habitation was very different than what we know today. It had a simple but prolific ecology that transitioned into a barren grassland. What factors caused the transition are unclear but are likely to be human r

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23

Becker, Bárbara Fernandes. "Evolução paleoambiental em salinas da Nhecolândia no holoceno superior, Pantanal sul-matogrossense." Universidade Federal de Mato Grosso, 2014. http://ri.ufmt.br/handle/1/588.

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Submitted by Simone Souza (simonecgsouza@hotmail.com) on 2017-11-07T13:33:04Z No. of bitstreams: 1 DISS_2014_Bárbara Fernandes Becker.pdf: 3053917 bytes, checksum: 060aed2f62884ff0f96ff9c066cf46de (MD5)<br>Approved for entry into archive by Jordan (jordanbiblio@gmail.com) on 2018-02-02T15:19:28Z (GMT) No. of bitstreams: 1 DISS_2014_Bárbara Fernandes Becker.pdf: 3053917 bytes, checksum: 060aed2f62884ff0f96ff9c066cf46de (MD5)<br>Made available in DSpace on 2018-02-02T15:19:28Z (GMT). No. of bitstreams: 1 DISS_2014_Bárbara Fernandes Becker.pdf: 3053917 bytes, checksum: 060aed2f62884ff0f96ff9c066

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Lazar, Kelly Best. "Benthic foraminifera as paleo-sea-ice indicators in the western Arctic Ocean." The Ohio State University, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=osu1417617424.

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25

Black, Manu School of Biological Earth &amp Environmental Sciences UNSW. "A late quaternary palaeoenvironmental investigation of the fire, climate, human and vegetation nexus from the Sydney basin, Australia." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2006. http://handle.unsw.edu.au/1959.4/25745.

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It is widely believed that Australian Aboriginals utilised fire to manage various landscapes however to what extent this impacted on Australia???s ecosystems remains uncertain. The late Pleistocene/Holocene fire history from three sites within the Sydney Basin, Gooches Swamp, Lake Baraba and Kings Waterhole, were compared with archaeological and palaeoclimatic data using a novel method of quantifying macroscopic charcoal, which is presented in this study. The palynology and other palaeoecological proxies were also investigated at the three sites. The Gooches Swamp fire record appeared to be mo

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26

Awad, Lara. "Dynamique des forêts de sapin de Cilicie au Liban et changements globaux : apports des analyses palynologiques et génétiques." Thesis, Montpellier 2, 2014. http://www.theses.fr/2014MON20087/document.

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Le Liban est un pays qui constitue un carrefour des civilisations. Depuis le temps des pharaons, ses ressources forestières ont été exploitées, notamment pour le commerce du bois. Le Liban, connu pour son cèdre, possède une autre espèce emblématique, le sapin de Cilicie, dont les forêts sont en majorité non protégées. Historiquement, le bois de sapin a été exploité durant le Nouvel Empire égyptien ancien pour la construction des temples et des navires. Il représentait ainsi un signe de pouvoir du pharaon, en formant notamment la barque d'Amon. De même, le sapin a été coupé pour la construction

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27

Avery, Graham. "Avian fauna, palaeoenvironments and palaeoecology in the late quaternary of the Western and Southern Cape, South Africa." Doctoral thesis, University of Cape Town, 1990. http://hdl.handle.net/11427/22441.

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Bibliography: pages 171-197.<br>Avian remains in coastal archaeological samples from Eland's Bay Cave, Die Kelders Cave 1 and Nelson Bay Cave in the Cape Province, South Africa, cover the periods between 80 000 and 40 000 B.P. and 18 000 and 300 B.P. Results of modern comparative surveys indicate that beached birds provide a predictable food supply. Kolmogorov-Smirnov two-sample nonparametric tests confirmed the close resemblance between the relative proportions of seabirds in archaeological and beached assemblages and earlier assumptions that the composition of seabird samples in archaeologic

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28

Balch, Deborah P. "Quaternary Ostracode Paleoecology and Its Link to Climate Change in the Bonneville Basin: A Detailed Study of the Glad800 Core GSL00-4, Great Salt Lake, Utah." Thesis, The University of Arizona, 2003. http://hdl.handle.net/10150/249251.

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We report the results of a detailed paleoecological study of the Bonneville Basin covering the last ~240,000 years. Our study used fossil ostracodes and a sedimentological record obtained from the August 2000 GLAD800 drilling operation at the Great Salt Lake. We analyzed 125 samples, taken at ~1 meter intervals from core GSL00-4, for ostracodes and other paleoecologic and sedimentological indicators of environmental change. Multivariate analyses applied to the ostracode data indicate an alternation between three major environments at the core site over the cored interval. The environments fluc

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29

De, Deckker P. "Australian Quaternary studies : a compilation of papers and documents submitted for the degree of Doctor of Science in the Faculty of Science, University of Adelaide /." Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SD/09sdd299.pdf.

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Figueroa, Rangel Blanca. "Long-term forest dynamics in high-altitude mountains of West-Central Mexico : the human and climate dimension in the Holocene." Thesis, University of Oxford, 2007. http://ora.ox.ac.uk/objects/uuid:30826402-1eb7-4d94-9a07-4d376c16eea0.

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This thesis presents the results of a study to examine long-term forest dynamics in the high-altitude mountains of West-Central Mexico. Vegetation dynamics on temporal scales ranging from 10<sup>2</sup> to 10<sup>3</sup> years were reconstructed in order to provide essential information on the temporal variability of ecological patterns and processes in these forests; information that is of direct relevance for their current and future conservation and management strategies. Vegetation and palaeoecological methods undertaken included fossil and modern pollen analysis, vegetation surveys, micro

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Barbour, Wood Susan L. "Quantitative Ecological and Taphonomic Patterns in Late Cenozoic Mollusk-Dominated Marine Fossil Assemblages." Diss., Virginia Tech, 2006. http://hdl.handle.net/10919/27710.

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Applications in paleontological research are far from being limited to taxonomic collection and identification. Nor is such research limited to working solely on fossil data. Actualistic paleontology is the study of modern or recent organisms and processes to better understand those of the past. The bulk of this body of research falls under the category of actualistic paleontology, and examines geochronological methods and error biases in dating biological specimens ranging in age from modern to thousands of years old. Although such methods are arguably not perfect, error rates of Â± a few

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Piva, Andrea <1978&gt. "High-resolution stratigraphy of Central and Southern Adriatic Quaternary deposits of sub-Milankovian climate change on Mediterranean circulation." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2007. http://amsdottorato.unibo.it/456/.

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This volume is a collection of the work done in a three years-lasting PhD, focused in the analysis of Central and Southern Adriatic marine sediments, deriving from the collection of a borehole and many cores, achieved thanks to the good seismic-stratigraphic knowledge of the study area. The work was made out within European projects EC-EURODELTA (coordinated by Fabio Trincardi, ISMAR-CNR), EC-EUROSTRATAFORM (coordinated by Phil P. E. Weaver, NOC, UK), and PROMESS1 (coordinated by Serge Bernè, IFREMER, France). The analysed sedimentary successions presented highly expanded stratigraphic interv

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Clemente, Iara Martins Matos Moreira. "Ecologia e paleoecologia de foraminíferos do holoceno na Baia de Guanabara, RJ." Universidade do Estado do Rio de Janeiro, 2011. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=9289.

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Este estudo teve como objetivo contribuir com as informações ecológicas e paleoecológicas geradas para a Baía de Guanabara com base na distribuição das assembléias de foraminíferos bentônicos. Para tal foram coletadas 30 amostras de sedimento superficial, ao longo de três perfis distribuídos pela baía e um testemunho (BG28) de 6 m de comprimento retirado próximo a Ilha do Governador. Nas amostras superficiais foram identificados 30 gêneros e 52 espécies das quais as espécies mais constantes foram Amonia tepida e Bolivina translucens que apresentaram a maior constância. Espécies de habitat de p

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Alin, Simone Rebecca. "Calibration and Interpretation of Holocene Paleoecological Records of Diversity from Lake Tanganyika, East Africa." Diss., The University of Arizona, 2001. http://hdl.handle.net/10150/231412.

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Lake Tanganyika is a complex, tropical ecosystem in East Africa, harboring an estimated 2,100 species. Extensive watershed deforestation threatens the biodiversity and ecological integrity of the lake. In this dissertation, ecological and paleoecological methods were employed to study the distribution of invertebrate biodiversity through space and time, with particular emphasis on linkages between biodiversity and land –use patterns. Ecological surveys of fish, mollusc, and ostracod crustacean diversity at sites in northern Lake Tanganyika representing different levels of watershed disturbance

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Petrocchi, Francesca. "Paleo- ecologia dei Foraminiferi in ambiente estremo: un caso di studio in Antartide." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amslaurea.unibo.it/9763/.

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Nel presente lavoro sono state analizzate le distribuzioni quantitative dei Foraminiferi planctonici e bentonici presenti in una carota e in un box core prelevati nel Mare di Ross in Antartide durante la campagna KOPRI ANTA03 nel Febbraio 2013 nell’ambito del progetto di ricerca congiunto Corea- Italia finanziato dal Progetto Nazionale di Ricerca in Antartide (PNRA). Scopo del lavoro è stato quello di comprendere l’evoluzione ambientale dell’area in base alla distribuzione quantitativa e qualitativa delle associazioni a Foraminiferi nel tardo Quaternario. In base alla distribuzione quantitati

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Schwartz, James P. "Late quaternary periplatform sediments and paleoenvironmental analysis of Pedro Channel, northeastern Nicaragua rise, Caribbean Sea." Thesis, 1996. http://hdl.handle.net/1911/14080.

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Using four periplatform sediment cores of intermediate water depth (900 to 1400 m) from the western Caribbean Sea, an investigation was conducted to ascertain the difference in cyclicity between the late-Brunhes Mode and the mid-Brunhes Mode. The past 185 ky define the late-Brunhes Mode, which records extreme changes between glacial and interglacial conditions, and consistent behavior within isotopic stages. Defined as 525 to 185 ky for the purposes of this study, the mid-Brunhes Mode represents a time of mild changes between and within glacial and interglacial stages, much like an extended la

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George, Christian Owens. "Alternative approaches to the identification and reconstruction of paleoecology of Quaternary mammals." 2012. http://hdl.handle.net/2152/19580.

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Since the 19th century the remains of Quaternary mammals were an important source of data for reconstructing past environmental conditions. I tested two basic assumptions that underlie Quaternary vertebrate paleoecology. The first assumption is that fossils mammals can be identified reliably to species. The second assumption is that correlations established between extant mammals and environmental parameters can be used to interpret reliably the paleoenvironment from the latest Pleistocene. Incorrect specimen identifications could lead to errors in paleoecologic interpretations. I explicitl

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Haddad, Geoffrey Allen. "Calcium carbonate dissolution patterns at intermediate water depths of the tropical oceans during the Quaternary." Thesis, 1994. http://hdl.handle.net/1911/16729.

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This study presents mineralogic and stable isotopic records generated for piston cores and Ocean Drilling Program holes recovered from intermediate water depths (500 to 2500 meters) near carbonate platforms around the world. Study areas included the Bahamas (western North Atlantic Ocean), the Nicaragua Rise (Caribbean Sea), the Maldives (north equatorial Indian Ocean), and the Queensland Plateau (southwest Pacific Ocean). Mineralogic data includes percent fine aragonite content, percent fine Mg calcite content, pteropod (aragonitic holoplanktonic gastropods) abundance, percent whole pteropods,

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39

SINGER, JILL KAREN. "TERRIGENOUS, BIOGENIC, AND VOLCANOCLASTIC SEDIMENTATION PATTERNS OF THE BRANSFIELD STRAIT AND BAYS OF THE NORTHERN ANTARCTIC PENINSULA: IMPLICATIONS FOR QUATERNARY GLACIAL HISTORY." Thesis, 1987. http://hdl.handle.net/1911/16106.

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A marine sedimentologic investigation was conducted on the northern Antarctic Peninsula continental margin. The data base included piston cores, surficial sediments, and high resolution seismic reflection profiles. The objectives of this study were three-fold: examine sedimentation patterns in the Bransfield Basin, a high-latitude, actively spreading back-arc basin; relate sedimentation processes to lithofacies patterns in bays and fjords of the South Shetland Islands, Palmer Archipelago, and Danco Coast; and interpret the recent glacial-climatic history of this region. As a back-arc basin in

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40

Marianelli, Pyramo C. "Palaeoenvironmental proxies from Southern Australian speleothems." Phd thesis, 2000. http://hdl.handle.net/1885/149912.

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41

Haberle, Simon. "Late quaternary environmental history of the Tari Basin, Papua New Guinea." Phd thesis, 1993. http://hdl.handle.net/1885/140965.

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42

Hellstrom, John Charles. "Late quaternary palaeoenvironmental records from the geochemistry of speleothems, North-West Nelson, New Zealand." Phd thesis, 1998. http://hdl.handle.net/1885/144671.

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43

De, Deckker P. (Patrick). "Australian Quaternary studies : a compilation of papers and documents submitted for the degree of Doctor of Science in the Faculty of Science, University of Adelaide." 2002. http://web4.library.adelaide.edu.au/theses/09SD/09sdd299.pdf.

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"April 2002" Includes bibliographical references and list of the publications and papers submitted. Pt. 1: section 1. Ostracod taxonomy and ecology -- section 2. Limnology of salt lakes -- section 3. Ostracod palaoecology - Quaternary environments -- section 4. Palaolimnology - Quaternary paleoenvironments and geology -- pt. 2: section 5. Geochemistry of ostracod shells -- section 6. Palaeoceanography Contains the majority of the author's scientific publications. Aims at reconstructing Quaternary paleoenvironments, mostly from the Australian region, using the fossil remains of organisms as wel

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44

Hickin, Adrian Scott. "Late Quaternary to Holocene Geology, Geomorphology and Glacial History of Dawson Creek and Surrounding area, Northeast British Columbia, Canada." Thesis, 2013. http://hdl.handle.net/1828/5100.

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Northeastern British Columbia was occupied by the Cordilleran (CIS) and the Laurentide (LIS) ice sheets, however, the timing and extent remains contentious. The late Quaternary and Holocene history of this area is examined by exploring geomorphic, stratigraphic, geochemical and geochronologic components of glacial, deglacial, paraglacial and non-glacial landsystems. New tools, such as GIS, LiDAR, and new geochronologic methods, such as optical dating are used to understand the Quaternary geology and geomorphology of the region. Bedrock topography represents the base of the Quaternary section

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45

Vollbrecht, Rüdiger Dr. "Postglazialer Anstieg des Meeresspiegels, Paläoklima und Hydrographie, aufgezeichnet in Sedimenten der Bermuda inshore waters." 1997. http://hdl.handle.net/11858/00-1735-0000-0006-B35B-4.

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