18% of Canada is covered in wetlands, and they comprise a
quarter of all the wetlands on earth! Canada’s wetlands include peatlands, a specific type of wetland also known as bogs
and fens, that produce peat (See SAM Blog "Know your Wetland Classes" to learn more about types of
wetlands!) In Newfoundland and Labrador, bogs and fens are very common and you
don’t have to go far in to get your boots stuck in thick peat.
Boots on the ground in the peat bog at Gosse's Pond Management Unit in Torbay, Newfoundland |
Climate change scientists have stated that peatlands are very
important when it comes to carbon sequestration. The Intergovernmental Panel on Climate Change (IPCC) have listed the restoration of peat soils as a mechanism
of mitigation against climate change. But what is peat and how is it formed? How does peat store carbon? And what can
we do as communities and individuals to advocate for climate change mitigation?
Peatland in Western Newfoundland |
Peat is composed almost entirely of decayed and decomposing
organic matter.
Depending on the peatland, the organic matter can be made up of different
mosses, sedges, and other herbaceous plants. When these plants die they
decompose very slowly. Decomposition rates vary across different peatlands, but
in general decomposition requires oxygen, and the waterlogged habitats of
peatlands reduce the amount of oxygen available, which in turn slows the
decomposition process. In northern wetlands the accumulation
of slowly decomposing peat happens over a millennia. According to a study at Laval University, it takes thousands of years to develop peat soils between 1.5
– 2.3m thick in northern peatlands. Most of the peatlands that exist
today were formed after the last ice age over 15,000 years ago.
In Newfoundland and Labrador a common type of peatland is a sphagnum
bog, made up of mostly sphagnum moss. Sphagnum has been referred to as a “bogbuilder” because of its ability to seemingly “create” the wetland.
Sphagnum moss in Pippy Park, St. John's, NL and diagram of individual sphagnum plant |
A Sphagnum bog is
made up of thousands of individual plants. The tops of the plants are exposed
to the sun and photosynthesize, meaning they use carbon dioxide to produce
sugars and food, and release oxygen as a bi-product. Sphagnum is very good at “bog building” or
creating peat because underneath the leaves on the surface are a long trails of dead
and decomposing leaves (See the brown leaves in the diagram on the right). These dead leaves are specialized to hold up to 3 times
their weight in water, which helps to facilitate an anaerobic peatland
environment, slow decomposition and the ‘building’ of bogs or peatlands.
Peatlands naturally expel carbon dioxide and methane, both
of which are greenhouse gases, but because the rate of decomposition is so
slow, they are able to store much more carbon and then they release, becoming a
carbon sink rather than a carbon source. It has been estimated that globally peatlands contain at least 550 Gt of Carbon which is double the amount stored in the world’s forests (see graph below for a comparison of carbon stored in terrestrial habitats!). Peatlands alone cover an estimated 3% of the world’s land area, but they
hold 30% of the terrestrial carbon.
Also, because it takes thousands of years for peatlands to develop they are
considered the most important long term carbon store in the terrestrial
biosphere. Some people consider peatlands to be the most efficient carbon sink on the
planet!
Carbon stored in terrestrial habitats Source; http://csites.eds.oinl.gov/faqs.html |
As amazing as they are, peatlands and wetlands are also very vulnerable to anthropogenic disturbance. Scientists have estimated that at least 64% of the world’s wetlands have disappeared since 1900. Pressures from agriculture, animal grazing, water diversion, infrastructure, and pollution are driving the loss of wetlands globally
So what happens if a
bog is disturbed? When peatlands are
burned or drained for (i.e. for agriculture) they go from being a carbon sink to a carbon source. According to an assessment of peatlands, biodiversity and climate change prepared
for the United Nations Environmental Programme, carbon dioxide emissions from peatland
fires, drainage and extraction is equal to 3000 million tonnes per annum or more
than 10% of all annual fossil fuel emissions per year. Without careful conservation the
mitigating effects of peatlands will be lost and the anthropogenic destruction
of peatlands will instead contribute to climate change.
To safeguard these incredible habitats, communities can take
action in many ways! For example, organizing clean ups in local wetlands can
help keep wetlands healthy and raise their public profile. Also, municipalities
and residents can show their support for wetland policies that promote the
sustainable use of wetlands and practice sustainable fishing, tourism, and
agriculture.
Municipal Representatives during the SAM Fall Meeting 2017 visiting the Corduroy Brook Nature Trail, a Management Unit in Grand Falls-Windsor, NL |
SAM communities have already taken the first step in
recognizing the values of wetlands by designating conservation areas within
their municipal boundaries. Let’s keep the momentum moving and become Wetland
Ambassadors by advocating for the sustainable use of wetlands to help mitigate
Climate Change!
So the next time your boot gets stuck in a bog when you are
looking for bakeapples remember, peatlands are doing their part to mitigate
climate change and by protecting them, we are doing our part for generations to
come! Join us next month and learn more about wetlands flood mitigating
properties in “Hold back the Gates: Wetlands mitigating flooding”! For more information on peatlands and climate change check out the resources below!
Resources:
1.
“Assessment on peatlands, biodiversity and
climate change: Executive summary” 2007 – 2008 UNEP-GEF http://ledsgp.org/wp-content/uploads/2015/12/Assessment-on-peatlands-biodiversity-and-climate-change-executive-summary.compressed.pdf
2.
Ayers, Peter. Field Bryology 110, http://rbg-web2.rbge.org.uk/bbs/activities/field%20bryology/FB110/FB110_Ayres_Sphagnum.pdf
3.
Barbier,
Edward, Mike Acreman and Duncan Knowler “Economic Valuation of Wetlands: A
guide for policy makers and planners” Ramsar Convention Bureau,
1997. https://www.ramsar.org/sites/default/files/documents/pdf/lib/lib_valuation_e.pdf
4.
Bengtsson,
Fia, Gustaf Granath, Hakan Rydin “Photosynthesis, growth, and decay traits in Sphagnum – A multispecies comparison”.
Ecology and Evolution, 2016 May 6(10):3325-3341. https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4833502/
5.
Ducks
Unlimited Canada “Researching Peatlands for Restoration” October 2015. http://www.ducks.ca/stories/boreal-forest/researching-and-restoring-peatlands/
6.
Government of
Canada, Environment and Natural Resources “Water Sources: Wetlands” https://www.canada.ca/en/environment-climate-change/services/water-overview/sources/wetlands.html
7.
Irish
Peatland Conservation Council, website “Sphagnum Moss – The Bog Builder” http://www.ipcc.ie/a-to-z-peatlands/sphagnum-moss-the-bog-builder/
8.
Hugron, Sandrine, Julie Bussieres and
Line Rochefort. “Tree plantations within the context of ecological restoration
of peatlands: practical guide. Peatland Ecology research group, Universite
Laval. 2013. http://www.gret-perg.ulaval.ca/uploads/tx_centrerecherche/Tree_Plantation_guide.pdf
9.
North
Carolina State University (NCSU) Water Quality Group. “Water Shedss: Functions
of Wetlands (Processes) http://www.water.ncsu.edu/watershedss/info/wetlands/function.html
10.
Intergovernmental
Panel on Climate Change (IPCC) “Climate Change 2007: Synthesis Report 4.
Adaptation and mitigation options. https://www.ipcc.ch/publications_and_data/ar4/syr/en/spms4.html
11.
Ovenden, Lynn. “Peat Accumulation in Northern Wetlands”
Science Direct, 1990. 33:3 Pg 377-386https://www.sciencedirect.com/science/article/pii/003358949090063Q?showall%3Dtrue%26via%3Dihub
12.
Ramsar Convention on Wetlands, Fact Sheet 8 “Keeping
Peatlands wet for a better future” 2015 https://www.ramsar.org/sites/default/files/documents/library/fs_8_peatlands_en_v5.pdf
13.
Ramsar Convention on Wetlands, Fact Sheet
3 “Wetlands: a global disappearing act” 2015 https://www.ramsar.org/sites/default/files/documents/library/factsheet3_global_disappearing_act_0.pdf
14.
Ramsar Convention on
Wetlands, Fact Sheet #1 “Wetlands: Why should I care?” 2015 https://www.ramsar.org/sites/default/files/documents/library/factsheet1_why_should_i_care_0.pdf
15.
Rice, S.K. “Mosses (Bryophytes)” Reference
module in earth systems and environmental science, Encyclopedia of inland
waters. 2009. Pages 88 – 96. https://www.sciencedirect.com/science/article/pii/B9780123706263002192
16.
Secretariat, North American wetlands
conservation council (Canada) “Wetlands Stewardship in Canada: Contributed
papers from the Conference on Canadian Wetlands Stewardship”. 2003/ Canadian
Wildlife Services, Environment Canada http://nawcc.wetlandnetwork.ca/Rep03-2e.pdf
Photos and images:
Image graph of carbon in terrestrial biomes: http://csite.eds.ornl.gov/faqs.html or http://ledsgp.org/wp-content/uploads/2015/12/Assessment-on-peatlands-biodiversity-and-climate-change-executive-summary.compressed.pdf
Image graph of carbon in terrestrial biomes: http://csite.eds.ornl.gov/faqs.html or http://ledsgp.org/wp-content/uploads/2015/12/Assessment-on-peatlands-biodiversity-and-climate-change-executive-summary.compressed.pdf
Photo of moss mat: D. Pelley, 2017, Pippy Park, NL
Photo of Lark Harbour Peatland, NL L. King, 2017, Lark
Harbour, NL
Photo of SAM Fall Meeting 2017 D. Pelley, 2017, Grand Falls-Windsor, NL