Sharing our Shoreline

Values and Views
Island Trust Communities
Marine By Nature
The Islands within the Salish Sea have been  shaped by ancient glaciers and modern oceanic forces. Whether you visit the islands seasonally or live here year round, Islanders treasure the marine environment.  The North Pender Local Trust Committee has developed this brochure to introduce you to where sensitive marine habitats exist, how you can recognize them, and what simple steps you can take to ensure our local waters continue to support a vibrant and abundant marine ecosystem.

This PDF has been produced by the North Pender Island Local Trust Committee: Sharing Our shorelines_lowres

IslandstrustContents:

Clean Water
Shoreline erosion
Coastal Bluffs and Shoreline beaches
Marine Riparian Vegetation
Intertidal Habitats
Beach-spawning Forage Fish
Eelgrass habitats
Kelp Forests and Rocky Reefs
Marine shorelines as critical fish habitats

Forage Fish in Metchosin

All articles and posts on the MetchosinCoastal website under the title Forage Fish may be found here:

In 2008 and in  2013, Ramona de Graaf, a biologist with the Public Education Program at the Bamfield Marine Station gave presentations on Forage Fish on our beaches  and the need to Document their occurrence. In 2008 on the Saturday after the presentation, we rejoined for a walk and a session on the process involved in sampling for Forage Fish on Taylor Beach. Ramona is also the principal and founding marine scientist of Emerald Sea Research and Consulting.

Our thanks from the Blue-Green Spaces committee to Ramona and Wen-Ling for this informative session on the importance of monitoring and preserving forage fish habitat.

See also the post: Overhanging Vegetation, Invertebrates and Forage fish

See also Forage Fish of Metchosin and Beyond by Moralea Milne with an article by Briony Penn : The herring, the Chinook and the Orca…At the Brink.  Moralea also documents a second training session by Ramona on Taylor Beach in March of 2009. Inclued is an article she wrote for the January Issue of The Metchosin Muse.

Throughout the Strait of Georgia, fish stocks have dramatically declined. Lingcod, rockfish and some Pacific salmon species are only some of the major commercial fish species in decline. Seabird populations throughout British Columbia and Washington State are also decreasing. As well, marine species such as the southern resident killer whale, dependent on salmon runs, have been listed as endangered. Many of these species depend on bait or ?forage? fishes as prey. Spawning habitat of forage fishes is located in nearshore marine environments, an environment heavily impacted by human development.

            Documenting and protecting forage fish spawning habitats must be a priority for the Metchosin Coastline.

There is little information on the current extent and health of the spawning habitats of herring and no information on the spawning habitat of surf smelt and Pacific sand lance. Surf smelt and sand lance spawn in gravel/sand beach habitats in the upper one third of the intertidal zone (Figure 1). Current spawning habitats of surf smelt and sand lance have been documented throughout the US coasts of the Juan de Fuca Strait, San Juan Islands, and Puget Sound (Penttila 2000, 2001). In Canada, eelgrass beds are protected as critical fish habitat under Fisheries and Oceans Canada ?no-net? loss policy (Federal Fisheries Act). Protecting forage fish spawning and rearing habitats will have positive benefits by protecting a vital food source for numerous marine predators. Fisheries and Oceans Canada recognizes the need to obtain information on the habitat requirements of forage fishes in Coastal areas.

intertidalzone

 

Intertidal zone spawning locations.
WHAT ARE WE CONCERNED ABOUT WITH METCHOSIN’S BEACHES?

Diversion of sediment-bearing streams through culverts, and the backshore and intertidal placement of seawalls, outfall pipes and riprap armouring interrupt natural coastal processes (such as erosion) that supply terrestrially-borne gravel sediments to beaches crucial to spawning surf smelt and Pacific sand lance. Seawalls are physical barriers that block the seaward transport of eroding gravels from feeder bluffs. Impediment of the long-shore transport of sediments by groins, outflow pipes, piers, boat ramps and docks have all contributed to the sediment-starved state of some beach faces. In general, the placement of seawalls and riprap armouring in the backshore and in the intertidal continues the process of sediment deprivation due to the action of wave scouring. Wave scouring can result in the loss of fine sands and gravels (appropriate for spawning) and the dominance of coarser (larger) gravels and cobble beaches inappropriate for use as spawning gravels for both surf smelt and Pacific sand lance. Seawalls such as those onPreliminary Habitat Assessment for suitability of intertidally spawning forage fish species, Pacific sand lance (Ammodytes hexapterus) and surf smelt (Hypomesus pretiosus) Esquimalt Lagoon, Colwood , British Columbia and Tower Point are often placed in the backshore, supralittoral and high intertidal zones (the uppermost portion of the high tide range) which can result in the loss of spawning habitat area, a decrease in beach elevation, an increase in beach slope, interruption of the sediment-transport drift cell, and the loss of sediment retaining logs. Not only are these ?hard? approaches to storm protection negatively impacting forage fish populations, but they can fail to deliver the protection intended. Around the world and locally, there are growing incidences of seawalls and other armouring failing to protect land owners. Modern engineering approaches, or ?soft? approaches work with coastal processes to provide safety for human populations and industries as well as maintaining marine ecological functions. While this report will not address this topic in detail, several informative websites and consultants include http://www.greenshores.ca, http://www.coastalgeo.com, and http:// www.sanjuans.org.
The presence of overhanging vegetation in marine riparian zones is important for the ecological function of nearshore marine habitats (Levings and Jamieson 2001; Brennan and Culverwell 2004) including having a positive effect on surf smelt spawn survival (Penttila 2001). The loss of overhanging vegetation (due to shoreline hardening measures) in the marine riparian zone has several ecological implications not only for marine fish and invertebrates, but the loss of shade cover increases the mortality of incubating surf smelt eggs (Penttila 2001, Rice 2006). Summer beach sediment temperatures are moderated by overhanging vegetation. Surf smelt eggs are typically anchored to surface gravels but are also buried between interstitial spaces within sediments layers (Penttila 2001). Surf smelt eggs deposited in summer months likely encounter high mortalities on the surface but eggs buried deeper in spawning substrates can avoid extreme surface temperatures and drying resulting in an increased survival rate (Penttila 2001). The loss of shading, however, increases thermal stress and desiccation to incubating eggs as temperatures within the sediments rise resulting in increased mortality of even buried eggs (Penttila 2001, Rice 2006). Vegetation buffers the drying effect of winds, and where beaches have lost riparian zones, eggs can also suffer a higher mortality than ?natural? due to wind-induced desiccation effects.
In Washington State, sand lance, surf smelt and other forage fish species such as anchovy are protected due to their importance to upper trophic levels of the food chain to support commercial fisheries (such as salmon, rockfish, ling god) and for ecosystem function (as advocated in WDFW principles of ecosystem management).

In general, surf smelt and Pacific sand lance depend on healthy nearshore and beach habitat, and they are vulnerable to impacts from shoreline development. Beaches with natural erosion processes supplying appropriate sized gravels and extant riparian zones are an optimal state for spawning surf smelt and sand lance. Winter spawning stocks of surf smelt may avoid desiccation stress and may have evolved to exploit beaches lacking overhanging vegetation (D. Penttila, pers. comm. 2007). Of primary importance for spawning is the mixture of gravels with a sand base. Cobbling beaches for heavy equipment operation, bulkheads, seawalls, outflow pipes and structures impeding sediment-transport drift cells are threats to maintaining these crucial spawning beaches.
The content of this report summarizes the data acquired from July 2006 to June 2007 (with mention of spawning results to September 07).The above was ADAPTED FROM RAMONA de GRAAF’S reference materials and the Forage Fish Report The photos above come from the Power Point presentation of Emerald Sea Research and Consulting. FORAGE FISH REPORT  The Boundary Bay intertidal forage fish spawning habitat report. Please contact Ramona and Wen-Ling of Forage Fish Matter! at emeraldsearesearch(use the at sign)hotmail.com or rdegraaf(use the at sign)bms.bc.ca for more information, talks or training!

 

Googlethe PDF : Preliminary Habitat Assessment for suitability of intertidally spawning forage fish species, Pacific sand lance (Ammodytes hexapterus) and surf smelt (Hypomesus pretiosus) Esquimalt Lagoon, Colwood , British Columbia

ALSO RAMONA HAS DONE A BEACH SPAWNING REPORT

 

Overhanging Vegetation, Invertebrates and Forage fish

Development along shorelines can very easily destroy or alter the natural coastal ecosystems so that the food supply and habitat maintenance of Forage Fish is affected negatively. Ramona de Graff has made several presentations on the importance of Forage Fish and has encouraged local residents to join in the documentation of occurrence of eggs on beaches.
From The Islands Trust “Sharing our Shorelines”
page 6: Shorelines Connect – Linking The Land And The Sea
Marine Riparian Vegetation
What is marine riparian vegetation?
The term “marine riparian” vegetation refers to grasses, shrubs, trees and logs lining marine shorelines. Marine riparian zones link the land and the sea through the exchange of water, sediments and nutrients.
Where is marine riparian vegetation located?
Vegetation above the high water mark, within “backshore” areas such as
private shoreline properties, on bluff tops and slopes form the marine
riparian zone.
Why is marine riparian vegetation important?
Insects captured by the winds as “wind fall” from shoreline vegetation are critical
for young salmon growth. Removing overhanging shoreline vegetation from summer
surf smelt spawning beaches causes embryos to die. Vegetation removal reduces key prey for juvenilesalmon and can reduce surf smelt populations. Fish losses affect the entire food web. Vegetated buffer zones are a wildlife migratory corridor and leaf litter provides nutrients to stimulate marine plankton growth.
Maintaining shoreline vegetation is a net benefit to property owners as a free
“ecosystem service” limiting erosion and stabilizing slope soils. Trees and
shrubs absorb large volumes of rain water and filter pollutants. Vegetation
removal may cause large sediment loads to enter the ocean limiting light for eelgrass growth and clogging fish gills.
See also on this website: Land Plants of Coastal Metchosin.

Ammodytes hexapterus: Pacific Sand lance, (Needle fish) : forage fish of Metchosin’s shoreline

See this post on Sandlance on Taylor Beach: gf-sandlance-july1320154

sandlance

Image from the  presentation below

One of the unusual characteristics of sandlance  on Taylor Beach is that in less  thAN a minute after emerging from the sand after spawning, If they are not consumed by crows or gulls, then they will die. ( so far I have not found this reported in the literature?)

Kingdom: Animalia
Phylum: Chordata
Class: Actinopterygii
Order: Perciformes
Family: Trachinoidea  (Bonaparte, 1832)
Genus: Ammodytes
Species: A. hexapteris
Binomial name Ammodytes hexapterus

Ramona de Graaf –2021 provides a good background on the importance of habitat for Forage Fish on our shores.

Marine and Estuarine Riparian Habitats and their role in Ecosystems in the Pacific Region

Canadian Science Advisory Secretariat Research Document 2001/109.

Colin Levings and Glen Jamieson, Fisheries and Oceans Canada

abstract
A.  introduction

in this paper we provide an assessment of the fish habitat significance of a particularly ecotone  of the Marine and estuary in Shoreline in British Columbia-locations were aquatic habitat at higher tides merges into terrestrial habitat. An eco-tone is defined as a son of transition between adjacent ecological systems, having a set of characteristics  uniquely defined by time and space scales, And by the strength of the interactions between adjacent ecological systems. Ecotones at the edges of lakes, streams, and rivers are well described by ecologists and are called riparian zones the word riparian is derived from the Latin word for River and is strongly embedded in ecological, legal, and environmental planning literature the following is a working definition of riparian habitat, adopted by DFO and MOV and parks in a recent document (2000) with fish habitat protection and area adjacent to a stream that may be subject to temporary, frequent, or seasonal inundation and supports plant species that are typical of an area inundated or saturated soil conditions, and that are distinct from plant species on freely drained adjacent upland sites because of the presence of water

See this PDF for the full article: MarineRiparianHabitats(LevingsJamieson2001)