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Tusket River & Basin
Tusket River & Basin Introduction The Tusket River presents an area of 3000 square kilometres (1158 square miles) on the southwestern tip of Nova Scotia. The area consists of a coastal basin with an inland watershed associated with the great Tusket River. This name is derived from a Mi'kmaq word "Neketaouksit" meaning "Great Forked Tidal River". This unique and diverse environment has offered natural resources to the Mi'kmaq First Nation's people for 7000 years and to the French Acadian settlers since the early 17th century. In the context of sustainable development, the present-day Acadians can offer a bilingual ecotourism package of nature-adventure and discovery blended with local history and heritage. The following natural history of the area will be presented in two segments. The first section will describe the natural environment of the Tusket Basin and its interrelationships with the Acadian people. The second segment will describe the natural history of the Tusket River in a similar manner to present the Acadian in his natural environment. Basin description 1. Physical features The Tusket Basin has a width of 32 kilometres (20 miles) between headlands at Chebogue Point and Lower East Pubnico. The mainland coastline between these two boundaries is highly indented and irregular with a measure of 500 kilometres (310 miles). Elongated points, peninsulas, ridges, drumlins (low hills) and eskers are oriented North-South and are separated by many tidal channels, inlets, estuaries and bays. High tide in the estuary of the "great forked tidal river" (Tusket) carries salt water inland for 24 kilometres (15 miles). -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
Lady Crabs, Ovalipes Ocellatus, in the Gulf of Maine
18_04049_CRABnotes.qxd 6/5/07 8:16 PM Page 106 Notes Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine J. C. A. BURCHSTED1 and FRED BURCHSTED2 1 Department of Biology, Salem State College, Salem, Massachusetts 01970 USA 2 Research Services, Widener Library, Harvard University, Cambridge, Massachusetts 02138 USA Burchsted, J. C. A., and Fred Burchsted. 2006. Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine. Canadian Field-Naturalist 120(1): 106-108. The Lady Crab (Ovalipes ocellatus), mainly found south of Cape Cod and in the southern Gulf of St. Lawrence, is reported from an ocean beach on the north shore of Massachusetts Bay (42°28'60"N, 70°46'20"W) in the Gulf of Maine. All previ- ously known Gulf of Maine populations north of Cape Cod Bay are estuarine and thought to be relicts of a continuous range during the Hypsithermal. The population reported here is likely a recent local habitat expansion. Key Words: Lady Crab, Ovalipes ocellatus, Gulf of Maine, distribution. The Lady Crab (Ovalipes ocellatus) is a common flats (Larsen and Doggett 1991). Lady Crabs were member of the sand beach fauna south of Cape Cod. not found in intensive local studies of western Cape Like many other members of the Virginian faunal Cod Bay (Davis and McGrath 1984) or Ipswich Bay province (between Cape Cod and Cape Hatteras), it (Dexter 1944). has a disjunct population in the southern Gulf of St. Berrick (1986) reports Lady Crabs as common on Lawrence (Ganong 1890). The Lady Crab is of consid- Cape Cod Bay sand flats (which commonly reach 20°C erable ecological importance as a consumer of mac- in summer). -
Narraguagus River Water Quality Monitoring Plan
Narraguagus River Water Quality Monitoring Plan A Guide for Coordinated Water Quality Monitoring Efforts in an Atlantic Salmon Watershed in Maine By Barbara S. Arter BSA Environmental Consulting And Barbara Snapp, Ph. D. January 2006 Sponsored By The Narraguagus River Watershed Council Funded By The National Fish and Wildlife Foundation Narraguagus River Water Quality Monitoring Plan A Guide for Coordinated Water Quality Monitoring Efforts in an Atlantic Salmon Watershed in Maine By Barbara S. Arter BSA Environmental Consulting And Barbara Snapp, Ph. D. January 2006 Sponsored By The Narraguagus River Watershed Council Funded By The National Fish and Wildlife Foundation Narraguagus River Water Quality Monitoring Plan Preface In an effort to enhance water quality monitoring (WQM) coordination among agencies and conservation organizations, the Project SHARE Research and Management Committee initiated a program whereby river-specific WQM Plans are developed for Maine rivers that currently contain Atlantic salmon populations listed in the Endangered Species Act. The Sheepscot River WQM Plan was the first plan to be developed under this initiative. It was developed between May 2003 and June 2004. The Action Items were finalized and the document signed in March 2005 (Arter, 2005). The Narraguagus River WQM Plan is the second such plan and was produced by a workgroup comprised of representatives from both state and federal government agencies and several conservation organizations (see Acknowledgments). The purpose of this plan is to characterize current WQM activities, describe current water quality trends, identify the role of each monitoring agency, and make recommendations for future monitoring. The project was funded by the National Fish and Wildlife Foundation. -
2019 Bay of Fundy Guide
VISITOR AND ACTIVITY GUIDE 2019–2020 BAYNova OF FUNDYScotia’s & ANNAPOLIS VALLEY TIDE TIMES pages 13–16 TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia and New Brunswick. Ferries.ca Find Yourself on the Cliffs of Fundy TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Isle Haute - Bay of Fundy Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia Take the scenic route and fi nd yourself surrounded by the and New Brunswick. natural beauty and rugged charm scattered along the Fundy Shore. Find yourself on the “Cliffs of Fundy” Cape D’or - Advocate Harbour Ferries.ca www.fundygeopark.ca www.facebook.com/fundygeopark Table of Contents Near Parrsboro General Information .................................. 7 Top 5 One-of-a-Kind Shopping ........... 33 Internet Access .................................... 7 Top 5 Heritage and Cultural Smoke-free Places ............................... 7 Attractions .................................34–35 Visitor Information Centres ................... 8 Tidally Awesome (Truro to Avondale) ....36–43 Important Numbers ............................. 8 Recommended Scenic Drive ............... 36 Map ............................................... 10–11 Top 5 Photo Opportunities ................. 37 Approximate Touring Distances Top Outdoor Activities ..................38–39 Along Scenic Route .........................10 -
The Annapolis Basin Scallop Fishery: a Historical Perspective and 1993 Stock Assessment
Scientific Excellence • Resource Protection & Conservation • Benefits for Canadians Excellence scientifique • Protection et conservation des ressources • Bénéfices aux Canadiens DFO Library MPO - Bbliothèque III IIIIHIIIIJIIII II I/9-- - 12022666 The Annapolis Basin Scallop Fishery: A Historical Perspective and 1993 Stock Assessment E. L. Kenchington and M. J. Lundy Benthic Fisheries and Aquaculture Division Biological Sciences Branch Department of Fisheries and Oceans P.O. Box 550 Halifax, Nova Scotia B3J 2S7 1994 Canadian Manuscript Report of Fisheries and Aquatic Sciences No. 2230 5-é-/ 23 Fisheries Pêches 1+1 and Oceans et Océans Canada. Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribu- tion is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of the Department of Fisheries and Oceans, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in Aquatic Sciences and Fisherics Abstracts and indexed in the Department's annual index to scientific and technical publications. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports ( Biological Series) of the Fisherics Research Board of Canada. Numbers 901-1425 were issued as Manuscript Reports of the Fisheries Research Board of Canada. -
Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin
Bay of Fundy Estuary Profiles Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin The Annapolis Basin is a sub-basin of the Bay of Fundy along the northwestern shore of Nova Scotia and at the western end of the Annapolis Valley. The Annapolis River is the major water source flowing into the estuary. At the NB mouth of the estuary, a narrow channel known as the Digby Gut connects the 44 NS estuary to the Bay of Fundy. Annapolis Royal and Digby are the main communities along the shore of the estuary, and Kingston-Greenwood is within the catchment area. Near Digby, there is a ferry port that connects to Saint John, New Brunswick. The estuary also hosts a tidal power generating station, which is near Annapolis Royal. The economy within the catchment area is largely driven by agriculture. However, Estuary surface area 104.07 km2 there are also several shellfish and finfish aquaculture tenures, and some Width at estuary mouth 1.85 km commercial fisheries near the mouth of the estuary that largely target Shoreline length 200.63 km invertebrates such as crab, lobster, and clams that inhabit tidal mudflats. The Catchment area 2322.05 km2 extensive tidal mudflats within the estuary are important habitat for Shorebird colonies 2 shorebirds. Within the catchment area there is freshwater habitat for wood Protected area 94.81 km2 turtles, and two protected areas that overlap with the landward boundary of Paved roads 1028 km the estuary. Although the upper valley is primarily agricultural land, much of Aquaculture leases 10 the rest of the catchment area is covered by forest. -
A History of Oysters in Maine (1600S-1970S) Randy Lackovic University of Maine, [email protected]
The University of Maine DigitalCommons@UMaine Darling Marine Center Historical Documents Darling Marine Center Historical Collections 3-2019 A History of Oysters in Maine (1600s-1970s) Randy Lackovic University of Maine, [email protected] Follow this and additional works at: https://digitalcommons.library.umaine.edu/dmc_documents Part of the Aquaculture and Fisheries Commons, History of Science, Technology, and Medicine Commons, and the United States History Commons Repository Citation Lackovic, Randy, "A History of Oysters in Maine (1600s-1970s)" (2019). Darling Marine Center Historical Documents. 22. https://digitalcommons.library.umaine.edu/dmc_documents/22 This Newsletter is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Darling Marine Center Historical Documents by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. A History of Oysters in Maine (1600s-1970s) This is a history of oyster abundance in Maine, and the subsequent decline of oyster abundance. It is a history of oystering, oyster fisheries, and oyster commerce in Maine. It is a history of the transplanting of oysters to Maine, and experiments with oysters in Maine, and of oyster culture in Maine. This history takes place from the 1600s to the 1970s. 17th Century {}{}{}{} In early days, oysters were to be found in lavish abundance along all the Atlantic coast, though Ingersoll says it was at least a small number of oysters on the Gulf of Maine coast.86, 87 Champlain wrote that in 1604, "All the harbors, bays, and coasts from Chouacoet (Saco) are filled with every variety of fish. -
2021 Striped Bass Regulations
2021 MAINE STRIPED BASS REGULATIONS If you are a recreational saltwater fisherman, Maine law may require you to register with the Maine Saltwater Recreational Fishing Registry. To learn more or to register visit: www.maine.gov/saltwater or call 207-633-9500. The following Maine saltwater recreational fishing regulations are current as of June 8, 2021. However, they are subject to change. Please contact our office or your local Marine Patrol Officer with questions. All minimum lengths are total length, NOT fork length. The sale of fish by recreational anglers is prohibited. Maine’s striped bass regulations cover all Maine coastal waters up to the head of tide in all rivers. In addition, there are special regulations in effect from December 1 through June 30 in the Kennebec, Sheepscot and Androscoggin Rivers and all related tributaries (see “SPECIAL KENNEBEC REGULATIONS” below). FEDERAL REGULATION It is unlawful to fish for, take or possess striped bass in Federal waters (waters greater than 3 miles from shore). STATEWIDE REGULATIONS OPEN SEASON January 1 through December 31, inclusive (except the Kennebec watershed, see below). BAG LIMITS A person may take and possess 1 fish per day. SIZE LIMITS The fish must be equal to or greater than 28 inches and less than 35 inches total length. “TOTAL LENGTH” is a straight line measurement from the lower jaw to the tip of the tail with the tail pinched together. DISPOSITION Personal use only, sale is prohibited. Fish must remain whole and intact. GENERAL GEAR RESTRICTIONS • Hook and line only, no gaffing of striped bass. • No bait allowed when using treble hooks. -
Dynamics of Larval Fish Abundance in Penobscot Bay, Maine
81 Abstract–Biweekly ichthyoplankton Dynamics of larval fi sh abundance surveys were conducted in Penobscot Bay, Maine, during the spring and early in Penobscot Bay, Maine summer of 1997 and 1998. Larvae from demersal eggs dominated the catch from late winter through spring, but Mark A. Lazzari not in early summer collections. Larval Maine Department of Marine Resources fi sh assemblages varied with tempera- P.O. Box 8 ture, and to a lesser extent, plankton West Boothbay Harbor, Maine 04575 volume, and salinity, among months. E-mail address: [email protected] Temporal patterns of larval fi sh abun- dance corresponded with seasonality of reproduction. Larvae of taxa that spawn from late winter through early spring, such as sculpins (Myoxocepha- lus spp.), sand lance (Ammodytes sp.), and rock gunnel (Pholis gunnellus) For most fi sh, the greatest mortality tial variation in species diver sity and were dominant in Penobscot Bay in occurs during early life stages (Hjort, abundance, and 3) to relate these vari- March and April. Larvae of spring to early summer spawners such as 1914; Cushing, 1975; Leggett and Deb- ations to differences in location and en- winter fl ounder (Pleuronectes america- lois, 1994). Therefore, it is essential that vironmental variables. nus) Atlantic seasnail (Liparis atlan- fi sh eggs and larvae develop in favorable ticus), and radiated shanny (Ulvaria habitats that maximize the probability subbifurcata) were more abundant in of survival. Bigelow (1926) recognized Materials and methods May and June. Penobscot Bay appears the signifi cance of the coastal shelf for to be a nursery for many fi shes; there- the production of fi sh larvae within the Field methods fore any degradation of water quality Gulf of Maine, noting that most larvae during the vernal period would have were found within the 200-m contour. -
Atlantic Coast
.............................................................. PAGE 181 Atlantic Coast I 0 81o 0 820 I§ 830 Iii 840 [j]jJ] 850 IIIIJ 860 ~ 870 • 880 • 890 I Figure 26: Region 800, Atlantic Coast, and its component Districts. Theme Regions: Natural History of Nova Scotia, Volume II PAGE .............................................................. 182 800 ATLANTIC COAST The Atlantic Coast Region is divided into nine Dis GEOLOGY tricts based upon major geomorphological charac teristics: The Atlantic Coast Region of Nova Scotia cuts across 810 Basalt Peninsula a great variety of rock types. 820 Cliffs and Beaches The Western Shore, South Shore, and Eastern 830 Beaches and Islands Shore (Districts 820, 830, and 840) are dominated by 840 Quartzite Headlands the old and generally very hard rocks of the Meguma 850 Granite Barrens Group. These are interfolded slates and greywackes, 860 Sedimentary Lowland with local outcroppings of metamorphosed volcanic 870 Till Plain ash and lava (Yarmouth area). Areas of very resistant 880 CUffed Island granite (District 850) also occur. In contrast, Cheda 890 Sandy Island bucto Bay has been eroded from weakly metamor phosed Carboniferous sandstones (District 860). Districts 830, 840, and 850 are further divided into Southeastern Cape Breton (District 870) is underlain Units based upon geomorphological, soil, and veg- by metamorphosed Precambrian volcanic ash de etation characteristics. · posits, sandstone, and granite. At the entrance to the Bay of Fundy, Digby Neck REGIONAL CHARACTERISTICS (District 810) is a low-lying basalt ridge. St. Paul Island (District 880) consists of very ancient Pre Exposure to winds from the Atlantic Ocean domi cambrian rocks similar to those found in the Cape nates coastal environments from Digby Neck to Breton massif. -
Atlantic Maritime Ecozone+: Evidence for Key Findings
Atlantic Maritime Ecozone+ evidence for key findings summary Canadian Biodiversity: Ecosystem Status and Trends 2010 Evidence for Key Findings Summary Report No. 3 Published by the Canadian Councils of Resource Ministers Library and Archives Canada Cataloguing in Publication Atlantic Maritime Ecozone+ evidence for key findings summary. Issued also in French under title: Sommaire des éléments probants relativement aux constatations clés pour l’écozone+ maritime de l’Atlantique. Electronic monograph in PDF format. En14-43/0-3-2015E-PDF 978-1-100-23826-5 Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: Exercise due diligence in ensuring the accuracy of the materials reproduced; Indicate both the complete title of the materials reproduced, as well as the author organization; and Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1- 800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Cover photos: Margaree Valley, Cape Breton Island, Nova Scotia, © iStock.com / cworthy; Hopewell Rocks, Bay of Fundy, New Brunswick, © iStock.com / MorganLeFaye This report should be cited as: ESTR Secretariat. 2014.