Holocene Climate History of British Columbia Using Pollen-Based Climate Reconstruction Techniques
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Neolithic and Early Bronze Age Environmental Background
Neolithic and Early Bronze Age Environmental Background 3 Neolithic and Early Bronze Age Environmental Background Keith Wilkinson and Vanessa Straker 3.1 Introduction similarly suggests that mean summer temperature may The Neolithic and Early Bronze Age periods both fall have been 2–3°C higher during the Neolithic, although within the middle of the Holocene geological series he also points out that loss of some indicator species (equivalent to the Flandrian stage, RL Jones and Keen could have been caused by human habitat modifica- 1993, 208). In north-western Europe, the Holocene tion. has been sub-divided in a number of ways based on Relative sea level rise decelerated throughout the vegetation changes observed in palynological and plant Neolithic from the peak levels seen in the Early macrofossil records from peat bogs, including, in the Mesolithic (Haslett et al. 2001). Although the most case of the former, the Somerset Levels (Figure 3.1 on recently published Holocene sea level curve for the the next page). South West (Heyworth and Kidson 1982; Haslett et al. The Neolithic coincides with West’s (1980) Fl II– 1997b; 2001) lacks the detail of its counterparts for Fl III chronozones, in other words the early to late the east coast of England (Devoy 1979; Haggart 1995; temperate periods of the Holocene. Therefore, in Shennan and Andrews 2000), it does provide some West’s model, the Neolithic is seen as immediately indication of the magnitude of coastal changes in the post-dating the Holocene interglacial optimum. A Neolithic (Figure 3.2 on page 65). A separate sea further means of subdividing the Middle Holocene is level curve has been produced for the Isles of Scilly Godwin’s (1940) pollen zonation scheme (Figure 3.1 by Charles Thomas (1985, 17–34), but it lacks abso- on the following page). -
Copyrighted Material
INDEX See also Accommodations and Restaurant indexes, below. AKAL Airport, 79 GENERAL INDEX aby Bedwell Lake, 119 Alder Grove Trail, 68 B Backcountry Tours, 144 Alexander Mackenzie Heri- bbott, Mount, 225 Baden-Powell Trail, 44, 48 A tage Trail (Nuxalk–Carrier Abbott Ridge, 225 Baker, Mount, 60, 214 Grease Trail), 167, 168 Abbott Ridge Trail, Glacier Balancing Rock, 132, 134 Alpha Pool, 180 National Park, 222–225 Bald eagles Alpine Club of Canada, 252 Acadia Beach, 56 Meares Island, 116 American Automobile Asso- Access America, 257 Vancouver Island, 81 ciation (AAA), 14, 254 Accommodations. See also Bald Mountain, 175 American Camp (San Juan Accommodations Index Bandanas, 10 Island), 98–102 best mountain lodges, 4–5 Banff, 248 Amphitrite Lighthouse, 113 Canadian Rockies and the Bare Buns Run, 56 Angel Staircase Falls, 232 Kootenays hikes, Barely Legal Motorsports, Annual Discovery 251–252 144 Package, 13 Cariboo Country, 188–189 Barkerville, gold rush and, Antler Creek, 175 green-friendly, 15 174 Apex Lookout, 201 Okanagan Valley hikes, Barkerville to Summit Rock & Arbutus Trail, 38 216–217 Groundhog Lake, 172–175 Area codes, 254 toll-free numbers and Barkley Sound, 113 Asking Rock, 147 websites, 262 Barred Owl Path, 38 Association of Canadian Vancouver and the Sun- Bate Point, 110 Mountain Guides, 19 shine Coast, 72–75 BC Ferries, 30 Atlin Provincial Park, 180 Vancouver Island, 120–122 BC Orchard Industry Atlin Quest, 180 Whistler area, 149–150 Museum, (Kelowna), 192 ATM networks/cash Admiralty Trail, 54 Beach Access A (West Coast points, -
British Columbia Vegetation and Climate History with Focus on 6 Ka BP
Document generated on 10/01/2021 4:51 p.m. Géographie physique et Quaternaire British Columbia Vegetation and Climate History with Focus on 6 ka BP Histoire du climat et de la végétation de la Colombie-Britannique, notamment de la période de 6 ka BP Geschichte der Vegetation und des Klimas in British Columbia während des Holozäns, besonders um 6 ka v.u.Z. Richard J. Hebda La paléogéographie et la paléoécologie d’il y a 6000 ans BP au Canada Article abstract Paleogeography and Paleoecology of 6000 yr BP in Canada British Columbia Holocene vegetation and climate is reconstructed from pollen Volume 49, Number 1, 1995 records. A coastal Pinus contorta paleobiome developed after glacier retreat under cool and probably dry climate. Cool moist forests involving Picea, Abies, URI: https://id.erudit.org/iderudit/033030ar Tsuga spp., and Pinus followed until the early Holocene. Pseudotsuga menziesii DOI: https://doi.org/10.7202/033030ar arrived and spread in the south 10 000-9000 BP, and Picea sitchensis - Tsuga heterophylla forests developed in the north. T. heterophylla increased 7500-7000 BP, and Cupressaceae expanded 5000-4000 BP. Bogs began to See table of contents develop and expland. Modern vegetation arose 4000-2000 BP. There were early Holocene grass and Artemisia communities at mid-elevations and pine stands at high elevations in southern interior B.C. Forests expanded downslope and Publisher(s) lakes formed 8500-7000 BP. Modern forests arose 4500-4000 BP while lower and upper tree lines declined. In northern B.C. non-arboreal communities Les Presses de l'Université de Montréal preceded middle Holocene Picea forests. -
Spatiotemporal Nutrient Loading to Cultus Lake: Context for Eutrophication and Implications for Integrated Watershed-Lake Management
Spatiotemporal nutrient loading to Cultus Lake: Context for eutrophication and implications for integrated watershed-lake management by Annika Elsie Putt Research Project Submitted In Partial Fulfillment of the Requirements for the Degree of Master of Resource Management Report No. 591 in the School of Resource and Environmental Management Faculty of Environment Annika Elsie Putt 2014 SIMON FRASER UNIVERSITY Summer 2014 Approval Name: Annika Elsie Putt Degree: Master of Resource Management Project No.: 591 Title of Thesis: Spatiotemporal nutrient loading to Cultus Lake: Context for eutrophication and implications for integrated watershed-lake management Examining Committee: Chair: Sergio Fernandez Lozada Master of Resource Management Candidate Dr Andrew Cooper Senior Supervisor Associate Professor: School of Resource and Environmental Management Erland MacIsaac Supervisor Head, Fish-Forestry Research Program Fisheries & Oceans Canada Adjunct Professor: School of Resource and Environmental Management Dr Daniel Selbie Supervisor Head, Lakes Research Program Fisheries & Oceans Canada Adjunct Professor: School of Resource and Environmental Management Date Defended/Approved: April 3, 2014 ii Partial Copyright Licence iii Abstract Cultus Lake, British Columbia experiences significant anthropogenic nutrient loadings and eutrophication. If continued unabated, these stresses threaten the persistence of two resident species at risk (coastrange sculpin and Cultus Lake sockeye salmon) and the many ecosystem services provided by the lake. We constructed water and nutrient budgets for the Cultus Lake watershed to identify major sources of nitrogen and phosphorus loadings to the lake. A steady-state water quality model calibrated against current nutrient loadings and limnological data was then used to explore water quality changes in response to various scenarios of nutrient loading to the lake. -
Pollen-Based Paleoenvironmental and Paleoclimatic Change at Lake Ohrid (South-Eastern Europe) During the Past 500 Ka
Biogeosciences, 13, 1423–1437, 2016 www.biogeosciences.net/13/1423/2016/ doi:10.5194/bg-13-1423-2016 © Author(s) 2016. CC Attribution 3.0 License. Pollen-based paleoenvironmental and paleoclimatic change at Lake Ohrid (south-eastern Europe) during the past 500 ka Laura Sadori1, Andreas Koutsodendris2, Konstantinos Panagiotopoulos3, Alessia Masi1, Adele Bertini4, Nathalie Combourieu-Nebout5, Alexander Francke6, Katerina Kouli7, Sébastien Joannin8, Anna Maria Mercuri9, Odile Peyron8, Paola Torri9, Bernd Wagner6, Giovanni Zanchetta10, Gaia Sinopoli1, and Timme H. Donders11 1Dipartimento di Biologia Ambientale, Università di Roma “La Sapienza”, Rome, Italy 2Paleoenvironmental Dynamics Group, Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany 3Institute of Geography and Education, University of Cologne, Cologne, Germany 4Dipartimento di Scienze della Terra, Università di Firenze, Florence, Italy 5HNHP – Histoire naturelle de l’Homme préhistorique, UMR 7194 CNRS, Département de Préhistoire, Muséum national d’Histoire naturelle, Institut de Paléontologie Humaine, Paris, France 6Institute for Geology and Mineralogy, University of Cologne, Cologne, Germany 7Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece 8CNRS UMR 5554, Institut des Sciences de l’Evolution de Montpellier, Université de Montpellier, Montpellier, France 9Dipartimento di Scienze della Vita, Laboratorio di Palinologia e Paleobotanica, Università di Modena e Reggio Emilia, Modena, Italy 10Dipartimento di Scienze -
Holocene Chironomid-Inferred Salinity and Paleovegetation Reconstruction
Document generated on 10/02/2021 8:21 a.m. Géographie physique et Quaternaire Holocene chironomid-inferred salinity and paleovegetation reconstruction from Kilpoola Lake, British Columbia La salinité (déterminée par les chironomides) et la reconstitution paléovégétale du Kilpoola Lake (Colombie-Britannique) à l’Holocène Salzgehalt, bestimmt durch die Chironomidae, und Rekonstruktion der Paläovegetation des Kilpoola-Sees, British Columbia Mark L. Heinrichs, Ian R. Walker, Rolf W. Mathewes and Richard J. Hebda Volume 53, Number 2, 1999 Article abstract Salinity fluctuations in lakes of semi-arid regions have been recognised as URI: https://id.erudit.org/iderudit/004878ar indicators of paleoclimatic change and have provided a valuable line of DOI: https://doi.org/10.7202/004878ar evidence in paleoclimatic reconstruction. However, factors other than climate, including sedimentologic events, may also affect salinity. At Kilpoola Lake, See table of contents early postglacial freshwater chironomids (Microtendipes, Sergentia, and Heterotrissocladius) occur in the basal sediments and yield a chironomid-inferred salinity of <0.03 g/l. Higher salinities, ranging from 1.0 to Publisher(s) 3.5 g/l, with Cricotopus/Orthocladius and Tanypus (chironomids typical of saline environments) follow and, persist for most of the remainder of the Les Presses de l'Université de Montréal Holocene. An inferred 450% salinity increase (from 1.6 to 7.3 g/l) occurred in the sediment above the Mount Mazama tephra, followed by a return to the ISSN pre-Mount Mazama salinity. The early Holocene pollen spectra are typical of open steppe, but the post-Mazama Artemisia pollen percentages are 0705-7199 (print) exceptionally high and are associated with silty clays. -
Constraining the Age of Lateglacial and Early Holocene Pollen Zones
Constraining the age of Lateglacial and early Holocene pollen zones and tephra horizons in southern Sweden with Bayesian probability methods Wohlfarth, B., Blaauw, M., Davies, S., Andersson, M., Wastegard, S., Hormes, A., & Possnert, G. (2006). Constraining the age of Lateglacial and early Holocene pollen zones and tephra horizons in southern Sweden with Bayesian probability methods. Journal of Quaternary Science, 21(4), 321-334. https://doi.org/10.1002/jqs.996 Published in: Journal of Quaternary Science Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:06. Oct. 2021 JOURNAL OF QUATERNARY SCIENCE (2006) 21(4) 321–334 Copyright ß 2006 John Wiley & Sons, Ltd. Published online 28 March 2006 in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/jqs.996 Constraining the age of Lateglacial and early Holocene pollen zones and tephra horizons in southern Sweden with Bayesian probability methods B. -
Order of the Executive Director May 14, 2020
PROVINCE OF BRITISH COLUMBIA Park Act Order of the Executive Director TO: Public Notice DATE: May 14, 2020 WHEREAS: A. This Order applies to all Crown land established or continued as a park, conservancy, recreation area, or ecological reserve under the Park Act, the Protected Areas of British Columbia Act or protected areas established under provisions of the Environment and Land Use Act. B. This Order is made in the public interest in response to the COVID-19 pandemic for the purposes of the protection of human health and safety. C. This Order is in regard to all public access, facilities or uses that exist in any of the lands mentioned in Section A above, and includes but is not limited to: campgrounds, day-use areas, trails, playgrounds, shelters, visitor centers, cabins, chalets, lodges, resort areas, group campsites, and all other facilities or lands owned or operated by or on behalf of BC Parks. D. This Order is in replacement of the Order of the Executive Director dated April 8, 2020 and is subject to further amendment, revocation or repeal as necessary to respond to changing circumstances around the COVID-19 pandemic. Exemptions that were issued in relation to the previous Order, and were still in effect, are carried forward and applied to this Order in the same manner and effect. Province of British Columbia Park Act Order of the Executive Director 1 E. The protection of park visitor health, the health of all BC Parks staff, Park Operators, contractors and permittees is the primary consideration in the making of this Order. -
CLOUDBURST Cover Photo Contest
CLOUDBURST Black Tusk Meadows & Tuck Lake Trail Progress Ski Skills for the Backcountry Spearhead Traverse Summer Route—Almost FEDERATION OF MOUNTAIN CLUBS OF BC Fall/Winter 2012 The Federation of Mountain Clubs of British Columbia INDEX (FMCBC) is a non-profit organization dedicated to the About the FMCBC.……………………………… 3 conservation of and the accessibility to British Colum- bia’s backcountry wilderness and mountain areas President’s Report………………………………. 4 FMCBC News……………………………………... 4 Membership in the FMCBC is open to any club or individual who supports our vision, mission and purpose. Member fees go to- Recreation & Conservation………………………. 5 wards furthering our work to protect and preserve the backcountry Trail Updates…..……………………………….. 7 for non-motorized recreation users. Member benefits include a subscription to our Cloudburst newsletter, monthly updates Club Ramblings……………...…………………. 11 through our FMCBC E-News, and access to an inexpensive third- Club Activities and Updates……………………… 15 party liability insurance program. Cover Photo Story……………………………….. 18 Backcountry Skills……………….……………… 19 FMCBC Executive Literature of Interest……………..…………..….. 20 President: Scott Webster (VOC) Treasurer: Elisa Kreller (ACC-Van) Announcements……………….…………………. 23 Secretary: Mack Skinner (NSH) Past President: Brian Wood (BCMC) FMCBC Directors Dave King (ACC-PG, CR), Caroline Clapham (ACC-Van), Andrew Cover Photo submitted by Linda Bily Pape-Salmon (VISTA), Rob Gunn and Judy Carlson (AVOC), Check out page 18 for Francis St. Pierre and Brian Wood (BCMC), -
At Mahoney Lake, British Columbia, Canada 219 DOI 10.2478/Limre-2020-0021
Limnol. Rev. (2020)Fifty years 20, 4:of 219-227limnology (1969-2019) at Mahoney Lake, British Columbia, Canada 219 DOI 10.2478/limre-2020-0021 Fifty years of limnology (1969-2019) at Mahoney Lake, British Columbia, Canada Markus L. Heinrichs1,*, Ian R. Walker2, Ken J. Hall3, Jörg Overmann4, 5, Molly D. O’Beirne6 1 Department of Geography and Earth & Environmental Science, Okanagan College, 1000 K.L.O. Road, Kelowna, British Columbia V1Y 4X8, Canada, e-mail: [email protected] (*corresponding author) 2 Department of Biology and Department of Earth, Environmental and Geographic Sciences, University of British Columbia, Okanagan Campus, 3333 University Way, Kelowna, British Columbia V1V 1V7, Canada, e-mail: [email protected] 3 Department of Civil Engineering, Institute for Resources, Environment and Sustainability, University of British Columbia, 2329 West Mall, Vancouver, British Columbia V6T 1Z4, Canada, e-mail: [email protected] 4 Leibniz-Institut DSMZ- German Collection of Microorganisms and Cell Cultures, Inhoffenstraße 7B, 38124 Braunschweig, Germany, e-mail: [email protected] 5 Braunschweig University of Technology, Universitätsplatz 2, 38106, Braunschweig, Germany 6 Department of Geology and Environmental Science, 4107 O’Hara Street, University of Pittsburgh, Pittsburgh, PA 15260, United States of America, e-mail: [email protected] Abstract: Mahoney Lake is a small, meromictic saline lake in south-central British Columbia noted for its unique layer of purple sulfur bacteria. First examined in 1969, this lake has undergone physical, chemical, biological, and pre-historical research to generate an understanding of how the lake and its biota function have developed through time. Advances in understanding the sulfur transformations and bacterial nutrient cycling over the last fifty years have been prolific, resulting in the description of several new taxa. -
2012 Lower Fraser Valley Air Quality Monitoring Report
2012 Lower Fraser Valley Air Quality Monitoring Report This report was prepared by the staff of the Air Quality Policy and Management Division of Metro Vancouver. The analysis and report was prepared by Geoff Doerksen with support from Ken Reid and Julie Saxton. The monitoring network is operated and maintained by a team including Tim Jensen, Michiyo McGaughey, Fred Prystarz, Scott Wong, Alex Clifford, Dave Pengilly, Shawn Connelly, Barry Steuck, Bob Cochlan and Richard Visser. Published: May 2014. Several government partners are acknowledged for contributing to the monitoring network including: Fraser Valley Regional District, Environment Canada and BC Ministry of Environment. Other partners acknowledged for providing funding to the monitoring network are: Vancouver Airport Authority, Chevron Canada Ltd., BC Hydro, Kinder Morgan Canada, and Port Metro Vancouver. Questions on the report should be directed to [email protected] or the Metro Vancouver Information Centre at 604-432-6200. Contact us: Metro Vancouver Air Quality Policy and Management Division 4330 Kingsway, Burnaby, BC V5H 4G8 604-432-6200 www.metrovancouver.org Disclaimer and Conditions: 1. Permission is granted to produce or reproduce these data, or any substantial part of them, for personal, non-commercial, educational and informational purposes only, provided that the data are not modified or altered and provided that this disclaimer notice is included in any such production or reproduction. 2. While the information in these data is believed to be accurate, these data and all of the information contained therein are provided “as is” without warranty of any kind, whether express or implied. All implied warranties, including, without limitation, implied warranties of merchantability and fitness for a particular purpose, are expressly disclaimed by Metro Vancouver and the Fraser Valley Regional District. -
Palaeolithic and Mesolithic
Palaeolithic and Mesolithic 2 Palaeolithic and Mesolithic Robert Hosfield, Vanessa Straker and Paula Gardiner with contributions from Anthony Brown, Paul Davies, Ralph Fyfe, Julie Jones and Heather Tinsley 2.1 Introduction For the Palaeolithic periods the open-landscape archaeology is dominated by lithic scatters (predom- The South West contains a diverse variety of Palaeo- inantly of deeply buried artefacts, frequently in fluvial lithic and Mesolithic archaeology of differing degrees deposits, and particularly true in the Lower and of significance. This reflects the nature of the arch- Middle Palaeolithic), although occupation sites such as aeological material itself, the histories of research Hengistbury Head (Barton 1992) and Kent’s Cavern in different parts of the region and, with regard to (Campbell and Sampson 1971) are also present. the Palaeolithic period, the differential preservation For the Mesolithic, there are greater numbers of of Pleistocene landforms and deposits throughout the excavated sites (especially from Somerset), although region. One of the key features of the Palaeolithic surface or shallow sub-surface lithic scatters are still archaeology is the presence of a significant cave-based common, especially in the west. resource in south Devon and northern Somerset, which is unquestionably of national significance (see Overall, the Palaeolithic and Mesolithic archae- for example, Campbell and Sampson 1971; Tratman ology of this region is generally rather poorly known, et al. 1971; Bishop 1975; Harrison 1977; Straw 1995; reflecting an absence of robust geochronological 1996; Andrews et al. 1999). frameworks, the predominance of research into a handful of cave and open sites over the lithic scatter In terms of an open-landscape Palaeolithic record, resource (whether located on the surface or deeply there is an inevitable bias towards those areas with buried) and the absence of any major syntheses.