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Some Principles of the Use of Macro-Areas Language Dynamics &A
Online Appendix for Harald Hammarstr¨om& Mark Donohue (2014) Some Principles of the Use of Macro-Areas Language Dynamics & Change Harald Hammarstr¨om& Mark Donohue The following document lists the languages of the world and their as- signment to the macro-areas described in the main body of the paper as well as the WALS macro-area for languages featured in the WALS 2005 edi- tion. 7160 languages are included, which represent all languages for which we had coordinates available1. Every language is given with its ISO-639-3 code (if it has one) for proper identification. The mapping between WALS languages and ISO-codes was done by using the mapping downloadable from the 2011 online WALS edition2 (because a number of errors in the mapping were corrected for the 2011 edition). 38 WALS languages are not given an ISO-code in the 2011 mapping, 36 of these have been assigned their appropri- ate iso-code based on the sources the WALS lists for the respective language. This was not possible for Tasmanian (WALS-code: tsm) because the WALS mixes data from very different Tasmanian languages and for Kualan (WALS- code: kua) because no source is given. 17 WALS-languages were assigned ISO-codes which have subsequently been retired { these have been assigned their appropriate updated ISO-code. In many cases, a WALS-language is mapped to several ISO-codes. As this has no bearing for the assignment to macro-areas, multiple mappings have been retained. 1There are another couple of hundred languages which are attested but for which our database currently lacks coordinates. -
The Problem of . the Cochrane in Late Pleistocene * Chronology
The Problem of . the Cochrane in Late Pleistocene * Chronology ¥ GEOLOGICAL SURVEY BULLETIN 1021-J A CONTRIBUTION TO GENERAL GEOLOGY 4 - THE PROBLEM OF THE COCHRANE IN LATE PLEISTOCENE CHRONOLOGY By THOR N. V. KAKLSTROM .ABSTRACT The precise position of the Cochrane readvances in the Pleistocene continental chronology has long been uncertain. Four radiocarbon samples bearing on the age of the Cochrane events were recently dated by the U. S. Geological Survey. Two samples (W-241 and W-242), collected from organic beds underlying sur face drift in the Cochrane area, Ontario, are more than 38,000 years old. Two samples (W-136 and W-176), collected from forest beds near the base and middle of a 4- to 6-foot-thick peat section overlying glacial lake sediments deposited after ice had retreated north of Cochrane, have ages, consistent with stratigraphic position, of 6,380±350 and 5,800±300 years. These results indicate that the Cochrane area may have been under a continuous ice cover from before 36,000 until some time before 4500 B. C.; this conforms with the radiocarbon dates of the intervening substage events of the Wisconsin glaciation. The radiocarbon results indicate that the Cochrane preceded rather than followed the Altither- mal climatic period and suggest that the Cochrane be considered a Wisconsin event of substage rank. Presented geoclimatic data seemingly give a consistent record of a glaciation and eustatic sea level low between 7000 and 4500 B. C., which appears to corre late with the Cochrane as a post-Mankato and pre-Altithermal event. A direct relation between glacial and atmospheric humidity changes is revealed by com paring the glacioeustatic history of late Pleistocene and Recent time with inde pendently dated drier intervals recorded from Western United States, Canada, and Europe. -
Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea
Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea Kortekaas, Marloes 2007 Link to publication Citation for published version (APA): Kortekaas, M. (2007). Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea. Department of Geology, Lund University. Total number of authors: 1 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 Post-glacial history of sea-level and environmental change in the southern Baltic Sea Marloes Kortekaas Quaternary Sciences, Department of Geology, GeoBiosphere Science Centre, Lund University, Sölvegatan 12, SE-22362 Lund, Sweden This thesis is based on four papers listed below as Appendices I-IV. -
Effet Réservoir Sur Les Âges 14C De La Mer De Champlain À La Transition Pléistocène-Holocène : Révision De La Chronologie De La Déglaciation Au Québec Méridional
_57-2-3.qxd 31/08/05 16:17 Page 115 Géographie physique et Quaternaire, 2003, vol. 57, nos 2-3, p. 115-138, 6 fig., 4 tabl. EFFET RÉSERVOIR SUR LES ÂGES 14C DE LA MER DE CHAMPLAIN À LA TRANSITION PLÉISTOCÈNE-HOLOCÈNE : RÉVISION DE LA CHRONOLOGIE DE LA DÉGLACIATION AU QUÉBEC MÉRIDIONAL Serge OCCHIETTI* et Pierre J.H. RICHARD*, respectivement : Département de géographie et Centre GEOTOP-UQAM-McGILL, Université du Québec à Montréal, C.P.8888, succursale Centre-ville, Montréal, Québec H3C 3P8 et Département de géogra- phie, Université de Montréal, C.P.6128, succursale Centre-ville, Montréal, Québec H3C 3J7. RÉSUMÉ L’âge de macrorestes de plantes ABSTRACT Reservoir effect on 14C ages of RESUMEN Datación con radiocarbono del terricoles et une extrapolation fondée sur le Champlain Sea at the Pleistocene-Holocene efecto reservorio del Mar de Champlain pollen des sédiments sous-jacents à la date transition: revision of the chronology of ice durante la transición Pleistoceno-Holoceno: basale du lac postglaciaire de Hemlock Carr retreat in southern Québec. Basal AMS-dates revisión cronológica de la desglaciación en el (243 m), au mont Saint-Hilaire, montrent que on terrestrial plant macrofossils coupled with Québec meridional. La edad de los macrores- la déglaciation locale y est survenue vers an extrapolation from the pollen content of tos de plantas terrestres y una extrapolación 11 250 ans 14C BP (13,3-13,1 ka BP). La underlying postglacial lake sediments at the fundada sobre el polen de los sedimentos datation croisée entre de tels macrorestes Hemlock Carr peatland (243 m), on subyacentes al estrato basal del lago postgla- (10 510 ± 60 ans 14C BP) et des coquilles de Mont Saint-Hilaire, show that local ice retreat ciar de Hemlock Carr (243 m), en el Mont sédiments marins (~12 200 ans 14C BP) pié- occurred around 11 250 14C yr BP (13,3- Saint-Hilaire, muestran que la desglaciación gés au fond du lac Hertel (169 m), voisin, 13,1 ka BP). -
Geochemical Evidence of the Sources of Aeolian Sands and Their Transport Pathways in the Minqin Oasis, Northwestern China
Quaternary International 334-335 (2014) 165e178 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Geochemical evidence of the sources of aeolian sands and their transport pathways in the Minqin Oasis, northwestern China Xiaozong Ren a,b, Xiaoping Yang a,*, Zhenting Wang c, Bingqi Zhu d, Deguo Zhang a, Patrick Rioual a a Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China b University of Chinese Academy of Sciences, Beijing 100049, China c Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China d Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China article info abstract Article history: Identification of aeolian sand sources occurring in oases of desert environments is of great importance Available online 17 May 2014 for understanding desertification processes and for developing strategies for sustainable development in arid regions. Combined with wind data and hierarchical cluster analysis, we analyzed the spatial char- Keywords: acteristics of major and trace elements of sands sampled at the margins of the Minqin Oasis, north- Sand source western China and its adjacent deserts (the Badain Jaran Desert and the Tengger Desert), with the Aeolian process purpose to identify the aeolian sand sources -
Lake-Level Oscillation Based on Sediment Strata and Geochemical Proxies Since 11,000 Year from Tengger Nuur, Inner Mongolia, China
feart-08-00314 August 6, 2020 Time: 22:43 # 1 ORIGINAL RESEARCH published: 07 August 2020 doi: 10.3389/feart.2020.00314 Lake-Level Oscillation Based on Sediment Strata and Geochemical Proxies Since 11,000 Year From Tengger Nuur, Inner Mongolia, China Zhang Chengjun*, Zhang Li, Zhang Wanyi, Tao Yunhan, Liu Yang, Wan Xiangling, Zhang Zhen and Safarov Khomid College of Earth Sciences & Key Laboratory of Mineral Resources in Western China (Gansu Province), Lanzhou University, Lanzhou, China A 794-cm section was collected from Tengger Nuur in the Inner Mongolian Plateau. Accelerator mass spectrometry 14C data were determined to set an age-depth model after removing about 1920 years of the carbon reservoir effect. Based on the multi- proxies grain size, carbonate-content, total organic carbon-content, ratio of C/N, ratios Edited by: Liangcheng Tan, of Mg/Ca and Sr/Ca, and carbonate carbon and oxygen isotopes, paleoenvironmental Institute of Earth Environment, changes since the last deglaciation were reconstructed. Tengger Nuur was very shallow Chinese Academy of Sciences, China during the last deglaciation under a cool and wet climate, especially during the interval Reviewed by: of the cold Younger Dryas event. Although, temperature and humidity increased from Hao Long, Nanjing Institute of Geography the early Holocene (∼10,450–8750 cal a BP), low lake levels indicated that the summer and Limnology (CAS), China monsoon was not sufficiently strong to reach the modern monsoon boundary in Inner Qianli Sun, East China Normal University, China Mongolia. High monsoon precipitation caused lake expansion during 8750–5000 cal a *Correspondence: BP, but the lake level oscillated in a shallow state under high evaporation. -
(NSF) Directorate of Geosciences
NSF Proposal accepted for funding March 22, 2007 Target Program: National Science Foundation (NSF) Directorate of Geosciences (GEO): Division of Earth Sciences (EAR): Sedimentary Geology and Paleobiology (SGP) Program – proposal submitted July 16, 2006 – proposal accepted for funding March 22, 2007 Title: Consolidation and Calibration of the New England Varve Chronology (NEVC): An Annual Continental Record of Ice Dynamics and Terrestrial Change, 18-11.5 kyr BP John C. Ridge 617-627-3494 or 617-627-2890 Dept. of Geology [email protected] Tufts University Medford, MA 02155 1 1. Project Summary Intellectual merit. Rapid climate change events during deglaciation are closely linked to ice sheet, ocean, and atmosphere interactions. Understanding these interactions requires high resolution comparisons of climate and continental ice dynamics. Although general patterns of Laurentide Ice Sheet (LIS) variation have been discerned, they are not continuously resolved at a sub-century scale. This lack of continuous, high-resolution terrestrial glacial chronologies with accurate radiometric controls continues to be a limiting factor in understanding deglacial climate. Such records, especially from the southeastern sector of the LIS, can provide critical comparisons to N. Atlantic climate records (marine and ice core) and a rigorous test of hypotheses linking glacial activity to climate change. Consolidation of the New England Varve Chronology (NEVC), and development of its records of glacier dynamics and terrestrial change, is a rare opportunity to formulate a complete, annual-scale terrestrial chronology from 18-11.5 kyr BP. Glacial varve deposition, which is linked to glacial meltwater discharge, can be used to monitor ice sheet ablation and has a direct tie to glacier mass balance and climate. -
SEE, Is Composed of SEE Conservation and SEE Foundation (Officially Registered As“Beijing Entrepreneur Environment Protection Foundation”)
SEE, is composed of SEE Conservation and SEE Foundation (officially registered as“Beijing Entrepreneur Environment Protection Foundation”). SEE sets its the mission as to“unite in the spirit of entrepreneurship for a better environment”and the value to“revere the nature and strive for a sustainable development”. Founded on June 5th, 2004, SEE Conservation is the first non-governmental organization that was established by entrepreneurs who would take the social responsibility to protect the environment in China. In 2008, SEE Conservation initiated and established the SEE Foundation (officially registered as“Beijing Entrepreneur Environment Protection Foundation”), aiming at supporting and nurturing Chinese environmental NGOs, and establishing a social protection platform that entrepreneurs, NGOs and the public can all be collaborated in enhancing environmental protection and sustainable development. At the end of 2014, SEE Foundation was upgraded to be a public-raising foundation. Based on environment protection and public welfare development, it focuses on fighting against desertification, promoting green supply chains and pollution prevention, and ecosystem conservation and nature education. By the end of 2017, with over 803 entrepreneur members, SEE had established 15 regional project centers that had provided support to more than 450 Chinese environmental NGOs and individuals directly and indirectly. In the future, SEE would keep maximizing the value of its social platform to inspire the general public to participate in environmental protection, putting further efforts in advocating and integrating inputs from entrepreneurs and the society to fight for a better environment. 1 Content Messages 04 SEE in China 16 SEE in 2017 42 th From the 6 Chairman 04 Shenzhen-Hong Kong Project Center 18 Inner Mongolia Project Center 36 Events of the Year 44 From the 7th Chairman 06 Taiwan Project Center 20 Anhui Project Center 37 General Meeting 46 Inculcation of Goodness, Inheritance of East China Project Center 22 Henan Project Center 38 virtues. -
Late Weichselian and Holocene Shore Displacement History of the Baltic Sea in Finland
Late Weichselian and Holocene shore displacement history of the Baltic Sea in Finland MATTI TIKKANEN AND JUHA OKSANEN Tikkanen, Matti & Juha Oksanen (2002). Late Weichselian and Holocene shore displacement history of the Baltic Sea in Finland. Fennia 180: 1–2, pp. 9–20. Helsinki. ISSN 0015-0010. About 62 percent of Finland’s current surface area has been covered by the waters of the Baltic basin at some stage. The highest shorelines are located at a present altitude of about 220 metres above sea level in the north and 100 metres above sea level in the south-east. The nature of the Baltic Sea has alter- nated in the course of its four main postglacial stages between a freshwater lake and a brackish water basin connected to the outside ocean by narrow straits. This article provides a general overview of the principal stages in the history of the Baltic Sea and examines the regional influence of the associated shore displacement phenomena within Finland. The maps depicting the vari- ous stages have been generated digitally by GIS techniques. Following deglaciation, the freshwater Baltic Ice Lake (12,600–10,300 BP) built up against the ice margin to reach a level 25 metres above that of the ocean, with an outflow through the straits of Öresund. At this stage the only substantial land areas in Finland were in the east and south-east. Around 10,300 BP this ice lake discharged through a number of channels that opened up in central Sweden until it reached the ocean level, marking the beginning of the mildly saline Yoldia Sea stage (10,300–9500 BP). -
When the River Began—The Formation of River Motala Ström and Human Presence in the Early Holocene, Sweden
quaternary Article When the River Began—The Formation of River Motala Ström and Human Presence in the Early Holocene, Sweden Jonas Bergman 1,* , Anna Plikk 1 , Jens Heimdahl 1, Linus Hagberg 1, Fredrik Hallgren 2, Jan Risberg 3 and Fredrik Molin 1 1 The Archaeologists, National Historical Museums, 126 53 Hägersten, Sweden; [email protected] (A.P.); [email protected] (J.H.); [email protected] (L.H.); [email protected] (F.M.) 2 The Cultural Heritage Foundation, 722 12 Västerås, Sweden; [email protected] 3 Department of Physical Geography, Stockholm University, 106 91 Stockholm, Sweden; [email protected] * Correspondence: [email protected] Received: 3 July 2020; Accepted: 21 August 2020; Published: 29 August 2020 Abstract: In conjunction with the extensive archaeological projects conducted at the current outlet of Sweden’s second largest lake, Lake Vättern, macrofossil, pollen and diatom records have been studied from 14C-dated lake and river sediments from River Motala Ström in Motala and Lake Boren. These investigations have revealed sedimentary evidence of the Yoldia Sea regression, the Ancient Lake Vättern transgression, and the following stepwise river formation process. Around 9000 cal BC, two small kettlehole basins at Strandvägen and Kanaljorden became isolated from the Baltic basin. As the ice sheet retreated further north, the isostatic uplift isolated the Vättern basin from the Baltic basin. Due to the uneven isostatic uplift, the basin tilted toward the south, and the Ancient Lake Vättern transgression started in Motala. The threshold in Motala at 92.5 m a.s.l. was reached around 7200 cal BC, and River Motala Ström was formed. -
The Late Quaternary Development of the Baltic Sea
The late Quaternary development of the Baltic Sea Svante Björck, GeoBiosphere Science Centre, Department of Geology, Quaternary Sciences, Lund University, Sölveg. 12, SE-223 62 Lund, Sweden INTRODUCTION Since the last deglaciation of the Baltic basin, which began 15 000-17 000 cal yr BP (calibrated years Before Present) and ended 11 000-10 000 cal yr BP, the Baltic has undergone many very different phases. The nature of these phases were determined by a set of forcing factors: a gradually melting Scandinavian Ice Sheet ending up into an interglacial environment, the highly differential glacio-isostatic uplift within the basin (from 9 mm/yr to -1mm/yr; Ekman 1996), changing geographic position of the controlling sills (Fig. 1), varying depths and widths of the thresholds between the sea and the Baltic basin, and climate change. These factors have caused large variations in salinity and water exchange with the outer ocean, rapid to gradual paleographic alterations with considerable changes of the north-south depth profile with time. For example, the area north of southern Finland-Stockholm has never experienced transgressions, or land submergence, while the developmen south of that latitude has been very complex. The different controlling factors are also responsible for highly variable sedimentation rates, both in time and space, and variations of the aquatic productivity as well as faunal and floral changes. The basic ideas in this article follow the lengthy, but less up-dated version of the Baltic Sea history (Björck, 1995), a more complete reference list and, e.g., the calendar year chronology of the different Baltic phases can be found on: http://www.geol.lu.se/personal/seb/Maps%20of%20the%20Baltic.htm. -
In the Wake of Deglaciation - Sedimentary Signatures of Ice-Sheet Decay and Sea-Level Change
! "# "$%&%'($$) * * +%,( - ."" %% /( 0 * 1 ./-2+ .-2/ *./3 4 .34/ 4*./5 6 .6/ 47 ( .-2/ .34 6/ 5 * * * ( 4 7 *-2 ( -2 8 ! 0(6 70-*9 * - (: ;<'$=<$( 7( 7 0-* %%><$="&$( 7(3 * 70-.?%"(&( 7/ 9 ( - *34 3 .?%%( 7/ 7 * @ (6 7 5 34 (3 * @ 7 (6 A 34(6 @ ( ! 5B 9 5 C * @ 5B @ (6 . :/ *6* (6 D: - 0(@ @ * * - 5(6 5B @ ( !" "$%& 1EE ( ( E F G 1 1 1 1%<';$> 07:;#&;%##;#%>', 07:;#&;%##;#%>,% ! *%$>;% IN THE WAKE OF DEGLACIATION - SEDIMENTARY SIGNATURES OF ICE-SHEET DECAY AND SEA-LEVEL CHANGE Henrik Swärd In the wake of deglaciation - sedimentary signatures of ice-sheet decay and sea-level change Studies from south-central Sweden and the western Arctic Ocean Henrik Swärd ©Henrik Swärd, Stockholm University 2018 ISBN print 978-91-7797-163-4 ISBN PDF 978-91-7797-164-1 Cover: Sólheimajökull, Iceland. Photo: Henrik Swärd Printed in Sweden by Universitetsservice US-AB, Stockholm 2018 Distributor: Department of Geological Sciences, Stockholm University S.D.G. Abstract Lacustrine and marine sedimentary archives help