Blog Post 1: Observations

The site that I have selected to conduct my field study is a forested area near my home north of Squamish, BC. I first visited the site on August 28 just before 7:00 pm. The day was hot (~30°C) and sunny and there had been no precipitation since June so the vegetation was very dry.

The site is located mid-slope on a terraced/undulating hillside with a westerly aspect. The undulations in the slope are formed by almost regularly spaced rock outcrops. Less than 50 m downslope of the site is a hydro power transmission line and cut block. The site is located on public forest land that has been previously harvested. I chose an area of approximately 20 m by 20 m to be my study site.

The forest is mature and the canopy cover is approximately 35%. The dominant species is Douglas-fir while western redcedar and lodgepole pine are also present. The shrub cover is dense at approximately 85% and is largely dominated by salal. Other shrub species include red and black huckleberry, Saskatoon, and red elderberry, as well as seedlings of western redcedar. I noted bracken fern in the depressions between rock outcrops but no other herbaceous species. The outcrops were covered in mosses (total cover of approximately 40%), which I identified as step moss, big red stem, and broom moss.

While I was at the site, a family of Ruffed Grouse moved through the area. The mother stood guard on top of one of the rock outcrops while the 3 young moved around in the undergrowth. I sat quite still and a couple of them came within a couple of metres from me.

Some questions of interest about this site are:
1) whether the species composition and cover of mosses vary with the position (crest, slope, depression) and aspect on the rock outcrops;
2) whether there is a difference in stand composition with distance from the cut line downslope; and
3) an investigation into why western redcedar seemed to be the dominant regenerating species (i.e. the most seedlings) while Douglas-fir is the dominant tree species.

Blog Post 1 – Observations

Although I had a different location planned, I noticed the amount of life in the courtyard at TRU so I decided to switch my location. Therefore, the area I chose to observe is the courtyard on the TRU campus between Old Main, the library and the Clock Tower. The area is approximately 1 acre (measured with the scale on google maps), once you account for the cement walkways and buildings on it. The topography is very slight hills, filled with thick grass. There are human planted flower beds which include a variety of flowers and ornamental grasses. There are also a handful of trees left in the courtyard.

I first visited this courtyard in respect to this course on September 13th, 2017 at 10:36 am. It was around 20 degrees celsius. The sun was shining and the sky was clear however the was a slight wind.

In my field journal (click – ecology) I took notes on many bees and insects I saw. My first question would be, can this type of urban ecosystem support other larger organisms? Secondly, what is essential to provide a habitat in an urban environment? (e.g., is just a grass lawn enough, are flowers essential, are trees needed?). Lastly, what would be the main food source for these other organisms, if they are present? Aside from the pollen in the flowers for the bees.

Fall Flowers

I am planning on using the Guerin Creek area of the Thompson Rivers University campus in Kamloops, BC (see figure 1). I explored this region and found that it varies drastically in access to water sources, and I thought I could examine how the vegetation and pollinators differ as the proximity to the creek varies. Kamloops is a desert climate and it is currently the end of summer/beginning of fall. As I explored my area of interest I noticed all of these brilliant yellow flowers blooming. Rabbitbrush is a late flowering plant that supports a lot of pollinators through the fall season. They bloom from September-October, so I thought they could be the perfect topic for my field experiment. There are also wild yellow sunflowers blooming, and from my research so far it seems like they actually might be from the same genus as the rabbitbrush.

Figure 1. Thompson Rivers University and Guerin Creek in Kamloops, BC. The highlighted areas are those I will consider during my field experiment.

The vegetation includes sagebrush, wildflowers, and drought resistant grasses. It is a creek, so there is a fairly steep elevation grade difference as the proximity to the creek changes (see figure 2). I am thinking I could compare both vegetation at higher elevations and lower elevations both near water sources and farther from water sources. In the map, you can see the blue region near the creek, and the pink area further from the creek. I will look at blooming vegetation and pollinators in both areas.

Figure 2. A freehand diagram of the relative election change near Guerin Creek.

I will keep my observations during the day, between 10-2 and ensure that it isn’t too windy for the pollinators to collect and fly. I will also only observe on days where it isn’t overcast or raining.

A few questions about this area:

  1. How do the number and type of rabbitbrush pollinators vary closer to and farther from water sources?
  2. How do the pollinator types vary between the wild sunflowers and the rabbitbrush?
  3. How does elevation affect the pollinators of rabbitbrush?

Blog Post 1: Observations

The area that I have selected to observe is a portion of a community park in Scarborough, Toronto, Ontario, called Milliken District Park. The total area of this park is approximately 32 hectares. It is located northeast of Scarborough at coordinates 43.8292° N, 79.2708° W. The park has many paved trails, a large pond, and numerous trees. There is a forest found near the pond. Most of the trees found in this park are mature.

Majority of the area is flat, but there are some hills. There is a rather large pond that which houses many birds, swans and fishes. Looking into the pond I could see an accumulation of litter, and the water quality seems poor.

The park contains landscaped gardens, gazeboes and different water features. There are also three playgrounds, a splash pad, and a large field where people usually play sports. I often visit this area weekly on walks, as there is a nice paved path around and inside the park, providing individuals with an area to bike, rollerblade, and walk. My initial observations and data collection of the park was made on 26 April 2017 from 6:07pm to 8:34pm. It was a sunny but windy day, with the temperature being around 12oC. During the collection period, there were many children playing in the playground. There were some birds and black squirrels that I saw in the forest, and throughout the park.

The area is mostly covered in green grass and trees. There are mixtures of deciduous and coniferous trees present throughout the park. Around the pond and the forest I noticed more wild type vegetation growth (sedges, weeds, etc). As this is a community park, roads and houses surround the park, but there is a clear distinction through the use of fences and gates.

Based on my observations, three questions that are interesting and could form the subject of my research project are:

  1. How does the pond have an impact on the vegetation and plant distribution surrounding it?
  2. How do humans impact the land, especially with regards to plant distribution?
  3. Not everything present in this park is natural, much of it is manmade, and thus, how does this impact plant distribution and the adaptation of the animal species that reside in the area?

Blog Post 1: Observations

Field Research Project – Site Visit #1

  • Recorder: Brian Titaro
  • Location: Surrey Bend Regional Park, Surrey, British Columbia
  • Visit Date: 09-06-2017
  • Visit Time: 14:45
  • Weather: Smokey skies from forest fires, no wind, 25oC

My field research project location will be Surrey Bend Regional Park (SBRP) located in Surrey, British Columbia on the south shore of the Fraser River. Surrey Bend is managed by the Metro Vancouver Regional District and is 348 hectares in size. SBRP consists of 5km un-dyked shoreline, medium bench floodplain ecosystems, and the third largest relatively undisturbed bog in the region. Nearly 80% of the park is closed to public access and within the accessible area there are three main ecological communities in which I will perform my study.

Surrey Bend Regional Park

The first is the Entrance Area (49.195301oo  N, 122.728121o W) characterized by mowed grass fields, gravel parking lots, and old field habitat. The dominate vegetation includes Achillea millefolium, Lupinus spp., Secale cereal, Anaphalis margaritacea, and Grindelia stricta and ornamental Acer spp.

Entrance Area

The second site is an open Wetland Complex (49.198919o N, 122.730074o W ) with man-made sloughs built by the Transportation Investment Corporation (TICorp) as a compensation projection for the fisheries damage that took place during the construction of the Port Mann Bridge. The wetlands are dominated by Phalaris arundinacea and Spiraea douglasii, interspersed with small Picea sitchensis, Rubus spectabilis, and Alnus rubra that were planted as a re-vegetation project.

Wetland Complex

The third site is a dense, closed canopy Riparian Forest along the Fraser River (49.199970o N, 122.727928o W). The dominate tree species are Populus trichocarpa, Picea sitchensis and Alnus rubra, with Symphoricarpos albus, Rubus spectabilis, and Acer circinatum making up the shrub layer, and Rubus ursinus covering the forest floor.

Riparian Forest

After visiting the site, the topics I’m interested in further researching would be:

  1. Does the bird species diversity change between the three ecosystems listed above?
  2. What fish species are using the recently constructed sloughs and are there features within the sloughs to which they are attracted?
  3. Which of the three ecosystems listed above hosts the largest diversity of non-native, invasive plant species?

Blog 1: Observations

The area I have selected for my observations is Mount Nkwala. Mount Nkwala is a mountain that is located west of the city of Penticton in the Okanagan Valley of British Columbia. Mount Nkwala has many surrounding hiking and mountain biking trails. The trails begin at the top of West Bench, Penticton, and they lead to the top of Mount Nkwala. Many of the trails have views of Penticton and the south end of Okanagan Lake. The elevation of Mount Nkwala is 1019m, and the area is roughly 300 hectares. Its topography is mainly mountain slopes with very few flat areas. Its vegetation is very diverse, being mainly forested with areas of shrubs and rock.

Coordinates: 49.5286° N, 119.6411° W

Visited July 20, 2017 at 1pm.

Weather

28° C

Wind: 11 km/h

Questions

1) What animals inhabit the space? And, what effect do they have on the surrounding vegetation?

2) How is the vegetation effected by the people that hike and bike on the trails?

3) How does plant diversity change depending on the different slopes within the area?

Blog Post 1: Observations.

For my project I selected Uplands Park as my research site, specifically the beach. Uplands Park is a 76-acre property located in a suburban neighbourhood in Victoria BC. The park is full of woodland trails and undeveloped natural reserve land. Terrain is relatively flat throughout the park and drops off a little closer to the beach. The ground is mainly soil, with a transition to a rockier terrain closer to the beach. Vegetation varies throughout the park. Taller trees are localized in the interior whereas bushes and grasses line the outskirts and roads that pass through the park. The rocky beach on the eastern side is home to many different types of seaweed and sea life. Barnacles are dispersed along the rocks close to the water. There are many tide pools along the beach with small communities living in them.

August 17 2017.

11:00AM, 19ᵒC, mainly sunny, wind 4km/h, humidity 64%

 

Questions:

  1. Could barnacle characteristics such as size and density per unit area squared be correlated with different water exposure levels?
  2. Tide pools situated at different elevations, thus flooding frequency, seemed to contain quite different compositions of plants and animals. Could there be a correlation between species present in a tide pool community and the frequency in which the tide pool is flooded?
  3. Could the characteristics of the seaweed in the tide pools be influenced by frequency of flooding?

 

Blog Post 1. Observations

For my research project, I chose the site that is designated as a City Park. McArthur island park is an area of 51 ha based on the parks official website data. It is surrounded by a sub-urban environment but is separated from it by a corridor – river pocket that makes it an island and connects to the big land by two bridges and a bridge with deranges which appears to control the water level in spring. Unfortunately, I didn’t find any information on the origin of this river pocket (man-made or naturally occurring). The GPS data for the site is Latitude 50,6960; Longitude -120,3785. I visited the site on Saturday July 22 at 15:30 for the primeral assessment, the weather was +29°C with 18 km/h of western wind, and humidity of 62%. The site appears to be a highly disturbed area because it contains 23 sport facilities as well as biking routs and a golf course. Therefore, majority of the area is covered by the man-made loan grass, ratio of green cover to concrete from the maps appears to be 5:1. The area of interest was mainly located on the western part of the park. It is a line of wild growth on one side bordering with the river valley and on the other side boarders with the cycling route that is 3,5 meters wide and then with the golf and soccer court (circled on the picture attached). The water level drops significantly in late September, creating a solid ground that connects the island to the sub-urban areas until mid-April. On the northern part of the area of interest man-made butterfly garden was assessed as well indicated by a dot on the map.

The vegetation is majorly represented by birch trees Betulla, young willow trees Salix, burdocks Arctium, low area by the water is covered in Polytrichum communis, Psilotum and Tetraphis pellucida. Middle height area is majorally represented by rough horse tail Equisetum.

The butterfly garden contained Verbena, Delphiniums, tiger lilies, Fleabane, poppy flowers, common mullein, and yellow daisies.

Young deer prints were found on the sand by the water and later was confirmed by a young deer found on the site, also squirrels, crows, ducks and woodpeckers were spotted.

On the butterfly garden, cabbage white butterflies Pieris rapae, wool carder bees Anthidium manicatum, western leafcutter bee Megachile perihirta, honey bees mostly male drones Apis, yellow faced bumblebees Bombus vosnesenskii and mixed bumblebees Bombus mixtus were spotted according to “Common pollinators of British Columbia visual identification guide”. It was noticed that the composition of pollinators in a suburb area neighboring the island is highly different.

 

Questions:

  • Abundance of some pollinators species were highly outnumbered in the garden and their composition (richness) is very different from the one found in front yard gardens in the Suburbs, could urbanization gradient effect pollinator species composition?
  • Which other effects could have impact on the population of pollinators in the study area (humidity, temperature, shading by human created structures by the site?
  • What are the factors affecting the plant community composition on both sides of the river pocket as the vegetation is slightly different on both sides.

Blog Post #1: Observations Edmonton, Alberta

Date visited: 29-05-2017 at 19:28pm

Weather: Clear, sunny, +20

Location

My research project site is located in the river valley in Edmonton, Alberta, which has the largest expanse of urban parkland in North America. It is located on the southwest side of the city. The site is around 80m distance from Whitemud Creek, which drains into the North Saskatchewan river. The river is approximately 536m north of the site.

Latitude: 53.500707

Longitude: -113.558685

Area: approximately 5,624 m²

Elevation gain from base of creek to upper research area: approximately 28m

*Stats found using google earth

Topography

The site is located on the side of a valley wall. The terrain varies from very steep drops to flat areas with small ponds. There are small streams constantly flowing through the area, which are fed by a spring located at the top. The side of the valley is made up of limestone rock, which releases iron into the water. The soil next to the streams are bright red due to the formation of rust. There is a rudimentary path that cuts directly through the upper and lower area of the research site, but it is not well used. There is a small waterfall that runs down the lower half and empties into a marshy area, before draining into the Whitemud Creek.

Vegetation

The canopy is dominated by White Spruce (Picea glauca), Balsam Poplar (Populus balsamifera), and Paper Birch (Betula papyrifera). The forest floor is mostly shaded. Other woody species observed: Saskatoon (Amelanchier alnifolia), Dogwood (Cornus stolonifera).

One plant I observed is very rare to the Edmonton river valley – the Round-leaved Orchid (Amerorchis rotundifolia). Other herbaceous plants observed: Bunchberry (Cornus canadensis), Western Violet (Viola canadensis), Arctic Raspberry (Ribus arcticus), Blue Columbine (Aquilegia brevistyla).

Questions:

  1. How does the high iron content in the soil affect the plant diversity in the area?
  2. How does the plant diversity change with the slope?
  3. There are small ponds located in the area. How does the iron in the water affect pond life?

Blog Post 1: Observations

I have selected to observe Paul Lake in Kamloops, British Columbia. This is a Provincial Park in which the public is welcome to use the campground or the beach for recreational use. Paul Lake is lined with small mountains which are covered with conifers. The recreational site has a vast amount of grassy areas which slowly turns into a sandy beach as it connects to the water. I visited this site at 12pm on a Thursday (June 22, 2017) afternoon. It was apporximately 20 degrees celsius with  clouds covering the blue sky. At the Provincial Park I became curious about the water levels at Paul Lake and how they are affected in the differing seasons with the temperature changes and climate changes. I also began to wonder how wildlife, such as geese or bugs, are affected by the water level changes. More explicitly I came up with these three questions, (1) what are the causes of water level changes? (2) Has the water levels at Paul Lake shown the same general trends over the years? And (3) how do these causes affect wildlife inhabiting nearby areas?