Climatic Variability in Western Victoria
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The Paleoecology and Fire History from Crater Lake
THE PALEOECOLOGY AND FIRE HISTORY FROM CRATER LAKE, COLORADO: THE LAST 1000 YEARS By Charles T. Mogen A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Environmental Science and Policy Northern Arizona University August 2018 Approved: R. Scott Anderson, Ph.D., Chair Nicholas P. McKay, Ph.D. Darrell S. Kaufman, Ph.D. Abstract High-resolution pollen, plant macrofossil, charcoal and pyrogenic Polycyclic Aromatic Hydrocarbon (PAH) records were developed from a 154 cm long sediment core collected from Crater Lake (37.39°N, 106.70°W; 3328 m asl), San Juan Mountains, Colorado. Several studies have explored Holocene paleo-vegetation and fire histories from mixed conifer and subalpine bogs and lakes in the San Juan and southern Rocky Mountains utilizing both palynological and charcoal studies, but most have been at relatively low resolution. In addition to presenting the highest resolution palynological study over the last 1000 years from the southern Rocky Mountains, this thesis also presents the first high-resolution pyrogenic PAH and charcoal paired analysis aimed at understanding both long-term fire history and the unresolved relationship between how each of these proxies depict paleofire events. Pollen assemblages, pollen ratios, and paleofire activity, indicated by charcoal and pyrogenic PAH records, were used to infer past climatic conditions. Although the ecosystem surrounding Crater Lake has remained a largely spruce (Picea) dominated forest, the proxies developed in this thesis suggest there were two distinct climate intervals between ~1035 to ~1350 CE and ~1350 to ~1850 CE in the southern Rocky Mountains, associated with the Medieval Climate Anomaly (MCA) and Little Ice Age (LIA) respectively. -
Corangamite Heritage Study Stage 2 Volume 3 Reviewed
CORANGAMITE HERITAGE STUDY STAGE 2 VOLUME 3 REVIEWED AND REVISED THEMATIC ENVIRONMENTAL HISTORY Prepared for Corangamite Shire Council Samantha Westbrooke Ray Tonkin 13 Richards Street 179 Spensley St Coburg 3058 Clifton Hill 3068 ph 03 9354 3451 ph 03 9029 3687 mob 0417 537 413 mob 0408 313 721 [email protected] [email protected] INTRODUCTION This report comprises Volume 3 of the Corangamite Heritage Study (Stage 2) 2013 (the Study). The purpose of the Study is to complete the identification, assessment and documentation of places of post-contact cultural significance within Corangamite Shire, excluding the town of Camperdown (the study area) and to make recommendations for their future conservation. This volume contains the Reviewed and Revised Thematic Environmental History. It should be read in conjunction with Volumes 1 & 2 of the Study, which contain the following: • Volume 1. Overview, Methodology & Recommendations • Volume 2. Citations for Precincts, Individual Places and Cultural Landscapes This document was reviewed and revised by Ray Tonkin and Samantha Westbrooke in July 2013 as part of the completion of the Corangamite Heritage Study, Stage 2. This was a task required by the brief for the Stage 2 study and was designed to ensure that the findings of the Stage 2 study were incorporated into the final version of the Thematic Environmental History. The revision largely amounts to the addition of material to supplement certain themes and the addition of further examples of places that illustrate those themes. There has also been a significant re-formatting of the document. Most of the original version was presented in a landscape format. -
Vict.. on HIS MAJESTY's SERVICE Geological Notebook No. 9
Cover ©Gill Estate. Except as otherwise indicated, the Gill Notebooks are copyright to the Gill Estate and licensed Western Dist. – Vict.. under a Creative Commons Attribution-NonCommercial- NoDerivatives 4.0 International License. ON HIS MAJESTY’S SERVICE Geological Notebook No. 9 National Museum of Victoria, Melbourne, C.I, Victoria, Australia Edmund D Gill Title page Notebook No. 9 If found please return to – Edmund D Gill Palaeontologist National Museum Russell Street Melbourne CI. 1951 Index 1 Lake Colongulac 3 “Chocolyn” bores 7 L. Colongulac levels 9 Analyses bore water 10 Tuff & loess 12 Loess cliffs 13 Camperdown Basalt 14 Winchelsea “laterite” 17 Sewerage outlet Dennington levels 19 Nestle’s 20 Levels Dennington Stn to Moulden’s Quarry 23 Moulden’s Q 25 Auger hole near Moulden’s Q 27 Levels M’s Quarry to coast 37 Excav. S.E. of Moulden’s Quarry Kelly Swamp 39 Excav. Merri Flats 40 Auger hole, bank Merri R. 41 Auger hole near Sanitary Depot 45 Dunes near Sanitary Depot 47 Tower Hill Beach 51 Goose Lagoon 53 Lake Gillear 54 Lake Gillear auger hole 55 Port Fairy drain 57 Holloway’s Beach 61 Levels Holloway’s Beach 67 Holloway’s Cave 70 Warrnambool 71 Thunder Pt. 72 Tower Hill Beach 74 Rd. ctg. E. of Illowa 75 Goose Lagoon 77 L. Colongulac 88 Queensland Museum 89 L. Keilambete 90 L. Connewarren, Mt. Shadwell, Mt. Elephant 91 Shelford 93 L. Colongulac 102 “Puunyart” Bore 103 L. Kariah L. Terangpom 104 Garvoc 107 Lake Terang 109 Lake Elingamite 111 Formation of calderas 112 Ewan’s Hill 113 Lake Purrumbeet 118 Camperdown Quarry south of Mt Leura 119 Mt Leura Camperdown 120 Quarries Camperdown 127 Rd. -
A Possible Late Pleistocene Impact Crater in Central North America and Its Relation to the Younger Dryas Stadial
A POSSIBLE LATE PLEISTOCENE IMPACT CRATER IN CENTRAL NORTH AMERICA AND ITS RELATION TO THE YOUNGER DRYAS STADIAL SUBMITTED TO THE FACULTY OF THE UNIVERSITY OF MINNESOTA BY David Tovar Rodriguez IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE Howard Mooers, Advisor August 2020 2020 David Tovar All Rights Reserved ACKNOWLEDGEMENTS I would like to thank my advisor Dr. Howard Mooers for his permanent support, my family, and my friends. i Abstract The causes that started the Younger Dryas (YD) event remain hotly debated. Studies indicate that the drainage of Lake Agassiz into the North Atlantic Ocean and south through the Mississippi River caused a considerable change in oceanic thermal currents, thus producing a decrease in global temperature. Other studies indicate that perhaps the impact of an extraterrestrial body (asteroid fragment) could have impacted the Earth 12.9 ky BP ago, triggering a series of events that caused global temperature drop. The presence of high concentrations of iridium, charcoal, fullerenes, and molten glass, considered by-products of extraterrestrial impacts, have been reported in sediments of the same age; however, there is no impact structure identified so far. In this work, the Roseau structure's geomorphological features are analyzed in detail to determine if impacted layers with plastic deformation located between hard rocks and a thin layer of water might explain the particular shape of the studied structure. Geophysical data of the study area do not show gravimetric anomalies related to a possible impact structure. One hypothesis developed on this works is related to the structure's shape might be explained by atmospheric explosions dynamics due to the disintegration of material when it comes into contact with the atmosphere. -
SCIENCE and SUSTAINABILITY Impacts of Scientific Knowledge and Technology on Human Society and Its Environment
EM AD IA C S A C I A E PONTIFICIAE ACADEMIAE SCIENTIARVM ACTA 24 I N C T I I F A I R T V N Edited by Werner Arber M O P Joachim von Braun Marcelo Sánchez Sorondo SCIENCE and SUSTAINABILITY Impacts of Scientific Knowledge and Technology on Human Society and Its Environment Plenary Session | 25-29 November 2016 Casina Pio IV | Vatican City LIBRERIA EDITRICE VATICANA VATICAN CITY 2020 Science and Sustainability. Impacts of Scientific Knowledge and Technology on Human Society and its Environment Pontificiae Academiae Scientiarvm Acta 24 The Proceedings of the Plenary Session on Science and Sustainability. Impacts of Scientific Knowledge and Technology on Human Society and its Environment 25-29 November 2016 Edited by Werner Arber Joachim von Braun Marcelo Sánchez Sorondo EX AEDIBVS ACADEMICIS IN CIVITATE VATICANA • MMXX The Pontifical Academy of Sciences Casina Pio IV, 00120 Vatican City Tel: +39 0669883195 • Fax: +39 0669885218 Email: [email protected] • Website: www.pas.va The opinions expressed with absolute freedom during the presentation of the papers of this meeting, although published by the Academy, represent only the points of view of the participants and not those of the Academy. ISBN 978-88-7761-113-0 © Copyright 2020 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form, or by any means, electronic, mechanical, recording, pho- tocopying or otherwise without the expressed written permission of the publisher. PONTIFICIA ACADEMIA SCIENTIARVM LIBRERIA EDITRICE VATICANA VATICAN CITY The climate is a common good, belonging to all and meant for all. -
Holocene Climatic Changes in the Westerly-Indian Monsoon Realm
https://doi.org/10.5194/cp-2020-141 Preprint. Discussion started: 17 November 2020 c Author(s) 2020. CC BY 4.0 License. Holocene climatic changes in the Westerly-Indian Monsoon realm and its anthropogenic impact Nicole Burdanowitz1, Tim Rixen1,2, Birgit Gaye1, Kay-Christian Emeis1,3 1Institute for Geology, Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany 5 2Leibniz-Zentrum für Marine Tropenforschung (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany 3Institute of Coastal Research, Helmholtz Center Geesthacht, Max-Planck-Straße 1, 21502 Geesthacht, Germany Correspondence to: Nicole Burdanowitz ([email protected]) Abstract. The Indian Summer Monsoon (ISM) with its rainfall is the lifeline for people living on the Indian subcontinent 10 today and possibly was the driver of the rise and fall of early agricultural societies in the past. Intensity and position of the ISM have shifted in response to orbitally forced thermal land-ocean contrasts. At the northwestern monsoon margins, interactions between the subtropical westerly jet (STWJ) and the ISM constitute a tipping element in the Earth’s climate system, because their non-linear interaction may be a first-order influence on rainfall. We reconstructed marine sea surface temperature (SST), supply of terrestrial material and vegetation changes from a very well-dated sediment core from the 15 northern Arabian Sea to reconstruct the STWJ-ISM interaction. The Holocene record (from 11,000 years) shows a distinct, but gradual, southward displacement of the ISM in the Early to Mid-Holocene, increasingly punctuated by phases of intensified STWJ events that are coeval with interruptions of North Atlantic overturning circulation (Bond events). -
Was the 4.2 Ka Event an Anthropogenic Disaster?
Open Journal of Ecology, 2016, 6, 613-631 http://www.scirp.org/journal/oje ISSN Online: 2162-1993 ISSN Print: 2162-1985 Was the 4.2 ka Event an Anthropogenic Disaster? Tomasz Jarosław Szczęsny Faculty of Political Science and International Studies, Nicolaus Copernicus University in Toruń, Toruń, Poland How to cite this paper: Szczęsny, T.J. Abstract (2016) Was the 4.2 ka Event an Anthropo- genic Disaster? Open Journal of Ecology, 6, The article describes a possible impact of demographic explosion during the Neolith 613-631. on local ecosystems and on the global climate as well as the role of this explosion in http://dx.doi.org/10.4236/oje.2016.610058 aggravating the course of 4.2 ka cooling event. A possible role of human activity in Received: July 27, 2016 changing the pattern of mid-latitudes westerlies, monsoons and Walker circulation Accepted: September 24, 2016 throughout the Holocene is analyzed. It is explained why during the Holocene Cli- Published: September 27, 2016 matic Optimum (HCO) monsoons could have been weaker than today, not stronger, as it is commonly stated. It is described how during the HCO the humid Tibetan Copyright © 2016 by author and Scientific Research Publishing Inc. Plateau could have repelled the Indian monsoon to the west and the East Asian This work is licensed under the Creative monsoon to the north. The explanation for weaker El Niño-Southern Oscillation Commons Attribution International (ENSO) during HCO is proposed. License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Keywords Open Access Holocene Climatic Optimum, Walker Circulation, Monsoon, Green Sahara Period, 4.2 ka Event 1. -
Multi-Proxy Reconstruction of South Asian Monsoon Variability in Sri Lanka
Multi-Proxy Reconstruction of South Asian Monsoon Variability in Sri Lanka Dissertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) vorgelegt dem Rat der Chemisch-Geowissenschaftlichen Fakultät der Friedrich-Schiller-Universität Jena von MPhil. Kasun Gayantha Henadheera Arachchige geboren am 23.05.1989 in Wathupitiwala, Sri Lanka Gutachter: 1. apl. Prof. Dr. Gerd Gleixner Max-Planck-Institut für Biogeochemie; FSU Jena 2. Prof. Dr. Roland Mäusbacher Institut für Geographie, FSU Jena Tag der Verteidigung: 14.07.2021 Dissertation, Friedrich-Schiller-Universität Jena, [2021] Acknowledgements First and foremost, I wish to extend my gratitude to my supervisors apl. Prof. Dr. Gerd Gleixner at the Max Planck Institute for Biogeochemistry (MPI-BGC), Jena, Prof. Dr. Achim Brauer at the German Research Centre for Geosciences (GFZ), Potsdam, Dr. Patrick Roberts at the Max Planck Institute for the Science of Human History (MPI-SHH), Jena, Prof. Joyanto Routh at Linköping University, Sweden, and Prof. Dr. Roland Mäusbacher at Friedrich- Schiller University, Jena. Without them, this thesis would not be possible, and I will always be immensely grateful for their guidance and advice throughout the process. I would also like to express my gratitude to Prof. Rohana Chandrajith, University of Peradeniya, Sri Lanka, apl. Prof. Dr. Peter Frenzel, IGW, Friedrich-Schiller University, Jena, and Dr. Anupama Krishnamurthy, French Institute of Pondicherry, India for their collaborations and support that have enabled me to enrich my datasets and expertise through training in novel methods. I thank them for taking the time out to teach me and allow me to develop my toolkit further. I would like to offer my special thanks to Dr. -
Volcano- and Climate-Driven Changes in Atmospheric Dust Sources And
Volcano- and climate-driven changes in atmospheric dust sources and fluxes since the Late Glacial in Central Europe Gaël Le Roux, Nathalie Fagel, Francois de Vleeschouwer, Michael Krachler, Vinciane Debaille, Peter Stille, Nadine Mattielli, Willem O. van der Knaap, Jacqueline F.N. van Leeuwen, William Shotyk To cite this version: Gaël Le Roux, Nathalie Fagel, Francois de Vleeschouwer, Michael Krachler, Vinciane Debaille, et al.. Volcano- and climate-driven changes in atmospheric dust sources and fluxes since the Late Glacial in Central Europe. Geology, Geological Society of America, 2012, vol. 40, pp. 335-338. 10.1130/G32586.1. hal-00915750 HAL Id: hal-00915750 https://hal.archives-ouvertes.fr/hal-00915750 Submitted on 9 Dec 2013 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Open Archive TOULOUSE Archive Ouverte (OATAO) OATAO is an open access repository that collects the work of Toulouse researchers and makes it freely available over the web where possible. This is an author-deposited version published in : http://oatao.univ-toulouse.fr/ Eprints ID : 9954 To link to this article : DOI: 10.1130/G32586.1 URL : http://dx.doi.org/10.1130/G32586.1 To cite this version : Le Roux, Gaël and Fagel, Nathalie and De Vleeschouwer, Francois and Krachler, Michael and Debaille, Vinciane and Stille, Peter and Mattielli, Nadine and Van der Knaap, Willem O. -
Heinrich Event - Wikipedia
Heinrich event - Wikipedia https://en.wikipedia.org/wiki/Heinrich_event Heinrich event A Heinrich event is a natural phenomenon in which large armadas of icebergs break off from glaciers and traverse the North Atlantic. First described by marine geologist Hartmut Heinrich (Heinrich, H., 1988), they occurred during five of the last seven glacial periods or "ice ages" over the past 640,000 years (Hodell, et al., 2008). Heinrich events are particularly well documented for the last glacial period but notably absent from the penultimate glaciation (Obrochta et al., 2014). The icebergs contained rock mass, which has been eroded by the glaciers, and as they melted, this material was dropped to the sea floor as ice rafted debris (abbreviated to "IRD"). The icebergs' melting caused extensive amounts of fresh water to be added to the North Atlantic. Such inputs of cold and fresh water may well have altered the density-driven, thermohaline circulation patterns of the ocean, and often coincide with indications of global climate fluctuations. Various mechanisms have been proposed to explain the cause of Heinrich events, most of which imply instability of the massive Laurentide ice sheet, a continental glacier covering north eastern North America during the last glacial period. Other northern hemisphere ice sheets were potentially involved as well (Fennoscandic, Iceland/Greenland). However, the initial cause of this instability is still debated. Contents Description Potential climatic fingerprint of Heinrich events Unusual Heinrich events Causes Internal forcings—the "binge–purge" model External forcings See also References Further reading External links Description The strict definition of Heinrich events is the climatic event causing the IRD layer observed in marine sediment cores from the North Atlantic: a massive collapse of northern hemisphere ice shelves and the consequent release of a prodigious volume of icebergs. -
South Tropical Atlantic Anti-Phase Response to Holocene Bond Events
South Tropical Atlantic anti-phase response to Holocene Bond Events Heitor Evangelista, Marcio Gurgel, Abdelfettah Sifeddine, Nivaor Rodolfo Rigozo, Mohammed Boussafir To cite this version: Heitor Evangelista, Marcio Gurgel, Abdelfettah Sifeddine, Nivaor Rodolfo Rigozo, Mohammed Bous- safir. South Tropical Atlantic anti-phase response to Holocene Bond Events. Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2014, 415, pp.21-27. 10.1016/j.palaeo.2014.07.019. insu- 01093711 HAL Id: insu-01093711 https://hal-insu.archives-ouvertes.fr/insu-01093711 Submitted on 15 Dec 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Palaeogeography, Palaeoclimatology, Palaeoecology 415 (2014) 21–27 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo South Tropical Atlantic anti-phase response to Holocene Bond Events Heitor Evangelista a,⁎, Marcio Gurgel e,f, Abdelfettah Sifeddine b,c, Nivaor Rodolfo Rigozo d, Mohammed Boussafir c a LARAMG – Laboratório de Radioecologia -
Multi-Decadal Climate Variability in Southern Iberia During The
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-158 Manuscript under review for journal Clim. Past Discussion started: 19 November 2018 c Author(s) 2018. CC BY 4.0 License. Multi-decadal climate variability in southern Iberia during the mid- to late- Holocene Julien Schirrmacher1,2, Mara Weinelt1, Thomas Blanz3, Nils Andersen2, Emilia Salgueiro4, Ralph R. Schneider1,2,3 1CRC 1266, Christian-Albrechts-Universität, Kiel, 24118, Germany 5 2Leibniz-Laboratory for Radiometric Dating and Stable Isotope Research, Christian-Albrechts-Universität, Kiel, 24118, Germany 3Department of Geosciences, Christian-Albrechts-Universität, Kiel, 24118, Germany 4Div. Geologica e Georecursos Marinhos, Instituto Português do Mar e da Atmosfera (IPMA), Lisbon, 1749-077, Portugal Correspondence to: Julien Schirrmacher ([email protected]) 10 Abstract. To assess the regional multi-decadal to multi-centennial climate variability at the southern Iberian Peninsula during the mid- to late- Holocene transition multi-proxy records of two marine sediment cores were established for two sites in the Alboran Sea (ODP-161-976A) and the Gulf of Cadiz (GeoB5901-2). High-resolution records of organic geochemical proxies and planktic foraminiferal assemblages are used to decipher precipitation and vegetation changes as well as the sea surface conditions with respect to Sea Surface Temperature (SST) and marine primary productivity (MPP). n-Alkane records as a proxy for precipitation changes suggest a series of six distinct drought events at 5.4 ka BP, 15 from ca. 5.1 ka BP to 4.9 ka BP, from 4.8 to 4.7 ka BP, at 4.6 ka BP, from 4.4 to 4.3 ka BP and, from 3.8 to 3.7 ka BP.