Accessing and Developing the Required Biophysical Datasets and Datalayers for Marine Protected Areas Network Planning and Wider Marine Spatial Planning Purposes
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North Sutherland Land Management Plan 2016-2026
North Sutherland Land Management Plan 2016-2026 North Highland Forest District North Sutherland Land Management Plan 2016 - 2026 Plan Reference No:030/516/402 Plan Approval Date:__________ Plan Expiry Date:____________ | North Sutherland LMP | NHFD Planning | North Sutherland Land Management Plan 2016-2026 Contents 4.0 Analysis and Concept 4.1 Analysis of opportunities I. Background information 4.2 Concept Development 4.3 Analysis and concept table 1.0 Introduction: Map(s) 4 - Analysis and concept map 4.4. Land Management Plan brief 1.1 Setting and context 1.2 History of the plan II. Land Management Plan Proposals Map 1 - Location and context map Map 2 - Key features – Forest and water map 5.0. Summary of proposals Map 3 - Key features – Environment map 2.0 Analysis of previous plan 5.1 Forest stand management 5.1.1 Clear felling 3.0 Background information 5.1.2 Thinning 3.1 Physical site factors 5.1.3 LISS 3.1.1 Geology Soils and landform 5.1.4 New planting 3.1.2 Water 5.2 Future habitats and species 3.1.2.1 Loch Shin 5.3 Restructuring 3.1.2.2 Flood risk 5.3.1 Peatland restoration 3.1.2.3 Loch Beannach Drinking Water Protected Area (DWPA) 5.4 Management of open land 3.1.3 Climate 5.5 Deer management 3.2 Biodiversity and Heritage Features 6.0. Detailed proposals 3.2.1 Designated sites 3.2.2 Cultural heritage 6.1 CSM6 Form(s) 3.3 The existing forest: 6.2 Coupe summary 3.3.1 Age structure, species and yield class Map(s) 5 – Management coupes (felling) maps 3.3.2 Site Capability Map(s) 6 – Future habitat maps 3.3.3 Access Map(s) 7 – Planned -
Ngu Report 2017.046
Geological Survey of Norway P.O.Box 6315 Torgard REPORT NO-7491 TRONDHEIM Tel.: 47 73 90 40 00 ISSN: 0800-3416 (print) Report no.: 2017.046 ISSN: 2387-3515 (online) Grading: Open Title: Seabed sedimentary environments and sediments (genesis) in the Nordland VI area off northern Norway Authors: Valérie K. Bellec, Reidulv Bøe, Client: MAREANO Leif Rise, Aave Lepland, Terje Thorsnes County: Norway Commune: Map-sheet name (M=1:250.000) Map-sheet no. and -name (M=1:50.000) Deposit name and grid-reference: Number of pages: 24 Price (NOK): 110,- Map enclosures: 0 Fieldwork carried out: Date of report: Project no.: Person responsible: 2008-2016 15.12.2017 311720 Summary: This report presents maps of sedimentary environments and seabed sediments (genesis) in the Nordland VI management area off northern Norway. The maps, which cover about 25 000 km² and water depths from 60 m to 2700 m, are based on multibeam echosounder data (bathymetry and backscatter), 215 video lines each 700 m long, seabed sediment samples from 40 stations (grab, boxcore and multicore) and 5500 km of sub-bottom profiler data. The sedimentary environment map has 6 classes, focussing on present depositional environments (erosion and deposition). Large parts of the Nordland VI continental shelf are dominated by erosion processes, but some deposition occurs in topographic depressions and glacial troughs like Trænadjupet and Vesterdjupet. Hemipelagic sediments are deposited in deep water areas on the continental slope and abyssal plain. The seabed sediments (genesis) map comprises a geological interpretation of the uppermost few metres of the seabed, and has 10 classes. -
Mozambique Channel, South-West Indian Ocean) E
Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean) E. Miramontes, S.J. Jorry, G. Jouet, J.W. Counts, S. Courgeon, P. Le Roy, C. Guerin, F.J. Hernández-Molina To cite this version: E. Miramontes, S.J. Jorry, G. Jouet, J.W. Counts, S. Courgeon, et al.. Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean). Sedimentology, 2019, 66 (4), pp.1222-1242. 10.1111/sed.12572. hal-02944583 HAL Id: hal-02944583 https://hal.archives-ouvertes.fr/hal-02944583 Submitted on 12 Apr 2021 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. 1 Sedimentology Article In Press Archimer https://archimer.ifremer.fr Acceptation date : 2018 https://doi.org/10.1111/sed.12572 https://archimer.ifremer.fr/doc/00472/58418/ Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean) Miramontes Elda 1, *, Jorry Stephan 2, Jouet Gwenael 2, Counts John 3, Courgeon Simon 4, Roy Philippe 1, Guerin Charline 2, Hernández-Molina F. Javier 5 1 UMR6538; CNRS-UBO; -
The Scottish Marine Protected Area Project – Developing the Evidence Base for Impact Assessments and the Sustainability Appraisal Final Report
Planning Scotland’s Seas The Scottish Marine Protected Area Project – Developing the Evidence Base for Impact Assessments and the Sustainability Appraisal Final Report Marine Scotland The Scottish Marine Protected Area Project – Developing the Evidence Base for Impact Assessments and the Sustainability Appraisal Final Report Date: July 2013 Project Ref: R/4136/1 Report No: R.2097 © ABP Marine Environmental Research Ltd Version Details of Change Date 1.0 Draft 29.04.2013 2.0 Draft 15.05.2013 3.0 Final 07.06.2013 4.0 Final 28.06.2013 5.0 Final 01.07.2013 6.0 Final 05.07.2013 Document Authorisation Signature Date Project Manager: S F Walmsley PP 05.07.2013 Quality Manager: C E Brown 05.07.2013 Project Director: S C Hull 05.07.2013 ABP Marine Environmental Research Ltd ABPmer is certified by: Quayside Suite, Medina Chambers, Town Quay, Southampton, Hampshire SO14 2AQ Tel: +44 (0) 23 8071 1840 Fax: +44 (0) 23 8071 1841 Web: www.abpmer.co.uk Email: [email protected] All images copyright ABPmer apart from front cover (wave, anemone, bird) and policy & management (rockpool) Andy Pearson www.oceansedgepzhotography.co.uk The Scottish Marine Protected Area Project – Developing the Evidence Base for Impact Assessments and the Sustainability Appraisal Summary Introduction The Marine (Scotland) Act and the UK Marine and Coastal Access Act contain provisions for the designation of a network of Marine Protected Areas (MPAs) in Scottish territorial and offshore waters in order to protect marine biodiversity and geodiversity and contribute to a UK and international network of MPAs. -
45. Sedimentary Facies and Depositional History of the Iberia Abyssal Plain1
Whitmarsh, R.B., Sawyer, D.S., Klaus, A., and Masson, D.G. (Eds.), 1996 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 149 45. SEDIMENTARY FACIES AND DEPOSITIONAL HISTORY OF THE IBERIA ABYSSAL PLAIN1 D. Milkert,2 B. Alonso,3 L. Liu,4 X. Zhao,5 M. Comas,6 and E. de Kaenel4 ABSTRACT During Leg 149, a transect of five sites (Sites 897 to 901) was cored across the rifted continental margin off the west coast of Portugal. Lithologic and seismostratigraphical studies, as well as paleomagnetic, calcareous nannofossil, foraminiferal, and dinocyst stratigraphic research, were completed. The depositional history of the Iberia Abyssal Plain is generally characterized by downslope transport of terrigenous sedi- ments, pelagic sedimentation, and contourite sediments. Sea-level changes and catastrophic events such as slope failure, trig- gered by earthquakes or oversteepening, are the main factors that have controlled the different sedimentary facies. We propose five stages for the evolution of the Iberia Abyssal Plain: (1) Upper Cretaceous and lower Tertiary gravitational flows, (2) Eocene pelagic sedimentation, (3) Oligocene and Miocene contourites, (4) a Miocene compressional phase, and (5) Pliocene and Pleistocene turbidite sedimentation. Major input of terrigenous turbidites on the Iberia Abyssal Plain began in the late Pliocene at 2.6 Ma. INTRODUCTION tured by both Mesozoic extension and Eocene compression (Pyrenean orogeny) (Boillot et al., 1979), and to a lesser extent by Miocene com- Leg 149 drilled a transect of sites (897 to 901) across the rifted mar- pression (Betic-Rif phase) (Mougenot et al., 1984). gin off Portugal over the ocean/continent transition in the Iberia Abys- Previous studies of the Cenozoic geology of the Iberian Margin sal Plain. -
Appendix 2 - Baseline Data Information and Maps
Appendix 2 - Baseline Data Information and Maps The information in this section represents baseline data which has been taken at either Highland wide level or, when available, Caithness and Sutherland level. Biodiversity, Flora and Key information Data Source Fauna Protect, enhance and There are currently 150 SSSI’s, 29 SNH website for information on where necessary restore SAC’s, 15 SPA’s, 4 NNR’s, 3 RAMSAR designated sites, site condition and designated wildlife sites in the Plan area. qualifying interests/features: and protected species www.snh.org.uk Scottish Biodiversity Strategy (Scotland’s Biodiversity - It’s In Your Hands; 2020 Challenge for Scotland’s Biodiversity) Flow Country, nominated to UNESCO The Peatlands of Caithness and as a tentative World Heritage Site, is a Sutherland - Management Strategy vitally important habitat on a regional 2005 - 2015 and international scale. It is the largest expanse of blanket bog in Europe, and covers about 4,000 km2 and home to a rich variety of wildlife, and is used as a breeding ground for many different species of birds. Improve biodiversity, Highland region supports 192 of the Highland Biodiversity Action Plan avoiding irreversible 238 priority species in Scotland and 40 www.highlandbiodiversity.com losses. of the 42 priority habitats. 455 of the priority species of conservation Habitat and Birds Directive – Annex importance are found in Highland. 1 Provide appropriate Proportion of population living within The Highland Councils Core path opportunities for people 200m of a footpath. The core paths plan. to come into contact with plan is yet to be completed but this and appreciate wild life information will be added to the and wild places. -
Dictionary of Geotourism Anze Chen • Young Ng • Erkuang Zhang Mingzhong Tian Editors
Dictionary of Geotourism Anze Chen • Young Ng • Erkuang Zhang Mingzhong Tian Editors Dictionary of Geotourism With 635 Figures and 12 Tables Editors Anze Chen Young Ng Chinese Academy of Geological Sciences The Geological Society of Australia Beijing, China Sydney, NSW, Australia Erkuang Zhang Mingzhong Tian The Geological Society of China China University of Geosciences Beijing, China Beijing, China ISBN 978-981-13-2537-3 ISBN 978-981-13-2538-0 (eBook) ISBN 978-981-13-2539-7 (print and electronic bundle) https://doi.org/10.1007/978-981-13-2538-0 Jointly published with Science Press, Beijing, China ISBN: 978-7-03-058981-1 Science Press, Beijing, China © Springer Nature Singapore Pte Ltd. 2020 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for gecneral use. The publisher, the authors, and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. -
Hybrid Turbidite-Drift Channel Complexes: an Integrated Multiscale Model A
https://doi.org/10.1130/G47179.1 Manuscript received 7 November 2019 Revised manuscript received 27 January 2020 Manuscript accepted 28 January 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 18 March 2020 Hybrid turbidite-drift channel complexes: An integrated multiscale model A. Fuhrmann1, I.A. Kane1, M.A. Clare2, R.A. Ferguson1, E. Schomacker3, E. Bonamini4 and F.A. Contreras5 1 Department of Earth and Environmental Sciences, University of Manchester, Williamson Building, Oxford Road, Manchester M13 9PL, UK 2 National Oceanography Centre, European Way, Southampton SO14 3HZ, UK 3 Equinor, Martin Linges vei 33, 1364 Fornebu, Norway 4 Eni Upstream and Technical Services, Via Emilia 1, 20097 San Donato Milanese, Milan, Italy 5 Eni Rovuma Basin, no. 918, Rua dos Desportistas, Maputo, Mozambique ABSTRACT sedimentological model for bottom current– The interaction of deep-marine bottom currents with episodic, unsteady sediment gravity influenced submarine channel complexes. flows affects global sediment transport, forms climate archives, and controls the evolution of continental slopes. Despite their importance, contradictory hypotheses for reconstructing past GEOLOGICAL SETTING flow regimes have arisen from a paucity of studies and the lack of direct monitoring of such The Jurassic to Paleogene basins offshore of hybrid systems. Here, we address this controversy by analyzing deposits, high-resolution sea- East Africa formed during the breakup of Gond- floor data, and near-bed current measurements from two sites where eastward-flowing gravity wana (Salman and Abdula, 1995). Following flows interact(ed) with northward-flowing bottom currents. Extensive seismic and core data Pliensbachian to Aalenian northwest-southeast from offshore Tanzania reveal a 1650-m-thick asymmetric hybrid channel levee-drift system, rifting, ∼2000 km of continental drift took place deposited over a period of ∼20 m.y. -
Beavers in Scotland a Report to the Scottish Government Beavers in Scotland: a Report to the Scottish Government
Beavers in Scotland A Report to the Scottish Government Beavers in Scotland: A report to the Scottish Government Edited by: Martin Gaywood SNH authors (in report section order): Martin Gaywood, Andrew Stringer, Duncan Blake, Jeanette Hall, Mary Hennessy, Angus Tree, David Genney, Iain Macdonald, Athayde Tonhasca, Colin Bean, John McKinnell, Simon Cohen, Robert Raynor, Paul Watkinson, David Bale, Karen Taylor, James Scott, Sally Blyth Scottish Natural Heritage, Inverness. June 2015 ISBN 978-1-78391-363-3 Please see the acknowledgements section for details of other contributors. For more information go to www.snh.gov.uk/beavers-in-scotland or contact [email protected] Beavers in Scotland A Report to the Scottish Government Foreword Beavers in Scotland I am delighted to present this report to Scottish Ministers. It is the culmination of many years of dedicated research, investigation and discussion. The report draws on 20 years of work on beavers in Scotland, as well as experience from elsewhere in Europe and North America. It provides a comprehensive summary of existing knowledge and offers four future scenarios for beavers in Scotland for Ministers to consider. It covers a wide range of topics from beaver ecology and genetics, to beaver interactions with farming, forestry, and fisheries. The reintroduction of a species, absent for many centuries, is a very significant decision for any Government to take. To support the decision- making process we have produced this comprehensive report providing one of the most thorough assessments ever done for a species reintroduction proposal. Ian Ross Chair Scottish Natural Heritage June 2015 Commission from Scottish Ministers to SNH, January 2014 Advice on the future of beavers in Scotland SNH should deliver a report to Scottish Ministers by the end of May 2015 summarising our current knowledge about beavers and setting out a series of scenarios for the future of beavers in Scotland. -
The Peatlands of Caithness & Sutherland
The Peatlands of Caithness & Sutherland MANAGEMENT STRATEGY The Peatlands of Caithness & Sutherland MANAGEMENT STRATEGY Contents # Foreword $ INTRODUCTION WHAT’S SO SPECIAL ABOUT THE PEATLANDS? $ # SO MANY TITLES % $ MANAGEMENT OF THE OPEN PEATLANDS AND ASSOCIATED LAND $ MANAGEMENT OF WOODLANDS IN AND AROUND THE PEATLANDS #$ % COMMUNITY AND ECONOMIC DEVELOPMENT #( ' SPREADING THE MESSAGE ABOUT THE PEATLANDS $ ( WHAT HAPPENS NEXT? $# Bibliography $$ Annex Caithness and Sutherland peatlands SAC and SPA descriptions $% Annex Conservation objectives for Caithness and Sutherland Peatlands SAC and SPA $' Acknowledgements $( Membership of LIFE Peatlands Project Steering Group $( Contact details for LIFE Peatlands Project funding partners $( Acronyms and abbreviations Bog asphodel Foreword As a boy I had the great privilege of spending my summers at Dalnawillan= our family home= deep in what is now called the “Flow Country” Growing up there it was impossible not to absorb its beauty= observe the wildlife= and develop a deep love for this fascinating and unique landscape Today we know far more about the peatlands and their importance and we continue to learn all the time As a land manager I work with others to try to preserve for future generations that which I have been able to enjoy The importance of the peatlands is now widely recognised and there are many stakeholders and agencies involved The development of this strategy is therefore both timely and welcome The peatlands of Caithness and Sutherland are a special place= a vast and -
Isolation of the South China Sea from the North Pacific Subtropical Gyre
www.nature.com/scientificreports OPEN Isolation of the South China Sea from the North Pacifc Subtropical Gyre since the latest Miocene due to formation of the Luzon Strait Shaoru Yin1*, F. Javier Hernández‑Molina2, Lin Lin3, Jiangxin Chen4,5*, Weifeng Ding1 & Jiabiao Li1 The North Pacifc subtropical gyre (NPSG) plays a major role in present global ocean circulation. At times, the gyre has coursed through the South China Sea, but its role in the evolutionary development of that Sea remains uncertain. This work systematically describes a major shift in NPSG paleo‑ circulation evident from sedimentary features observed in seismic and bathymetric data. These data outline two contourite depositional systems—a buried one formed in the late Miocene, and a latest Miocene to present‑day system. The two are divided by a prominent regional discontinuity that represents a major shift in paleo‑circulation during the latest Miocene (~ 6.5 Ma). The shift coincides with the further restriction of the South China Sea with respect to the North Pacifc due to the formation of the Luzon Strait as a consequence of further northwest movement of the Philippine Sea plate. Before that restriction, data indicate vigorous NPSG circulation in the South China Sea. Semi‑ closure, however, established a new oceanographic circulation regime in the latest Miocene. This work demonstrates the signifcant role of recent plate tectonics, gateway development, and marginal seas in the establishment of modern global ocean circulation. In the Pacifc Ocean, the North Pacifc subtropical gyre (NPSG) represents a surface level water mass that advects warm water from the tropics to central and higher-latitude areas of the North Pacifc basin. -
Book of Abstracts Vliz Young Marine Scientists’ Day
BOOK OF ABSTRACTS VLIZ YOUNG MARINE SCIENTISTS’ DAY VIVES, Brugge 20 February 2015 VLIZ SPECIAL PUBLICATION 71 - i - This publication should be quoted as follows: Jan Mees and Jan Seys (Eds). 2015. Book of abstracts – VLIZ Young Marine Scientists’ Day. Brugge, Belgium, 20 February 2015. VLIZ Special Publication 71. Vlaams Instituut voor de Zee – Flanders Marine Institute (VLIZ): Oostende, Belgium. xiv + 196 p. Vlaams Instituut voor de Zee Flanders Marine Institute VLIZ – InnovOcean site Wandelaarkaai 7 8400 Oostende, Belgium Tel. +32-(0)59-34 21 30 Fax +32-(0)59-34 21 31 E-mail: [email protected] http://www.vliz.be Photo cover: Sea view from the tallest building (Europe Center) of Ostend: view on the beach, the western dyke, and the RV Simon Stevin entering the port (August 2014) © VLIZ (Leontien De Wulf) Reproduction is authorized, provided that appropriate mention is made of the source. ISSN 1377-0950 - ii - PREFACE This is the ‘Book of Abstracts’ of the 15th edition of the VLIZ Young Marine Scientists’ Day, a one day event that was organised on 20 February, 2015 in VIVES, Brugge. This annual event has become more and more successful over the years. With more than 300 participants and circa 130 scientific contributions, it is fair to say that it is the place to be for Flemish marine researchers and for the end-users of their research. It is an important networking opportunity, where young scientists can meet and interact with their peers, learn from each other, build their personal professional network and establish links for collaborative and interdisciplinary research.