Paper · 1959 · ARCTIC

Bogs and Fens in the Hudson Bay Lowlands

Hugo Sjörs

5
claims
5
verbatim quotes
96
citations
2
research areas
✓
Open access

Abstract

Describes structural and vegetative features of bogs and fens in the peatlands area south and west of Hudson Bay, examined in summer 1957 mainly near the confluence of the Attawapiskat and Muketei Rivers (approx. 53 N, 86 W). Distinctive features of the ridge-shaped raised bogs are their undulating surfaces, large shallow pools, and lateral seepages (small, shallow pools termed flarks, in a stepped arrangement down the bog edges). Bog vegetation, typical of ombrotrophic peatlands, is acidophilous and low in pH value except in limited areas, e.g. fissures caused by frost heaving where fen plants are found, also the lateral seepages where patches of true fen vegetation appear along the rows of flarks. The plant communities are almost identical with those of similar raised bogs in Sweden and Finland. Fen surfaces are covered by large pools, and alternating low ridges low ridges and flarks. The fen water is highly minerotrophic, resulting in vegetation richer in mineral nutrients than that of the bogs, and similar to the "rich fen" or "brown fen" vegetation of Scandinavia. Roundish "black-spruce islands" are conspicuous fen features; they have permafrost cores as do knolls (palsas) north eastward near Sutton and Hawley Lakes.

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Claims 5

Observationobservedoriginal resultmeasured

Claim · model-written summary

Raised bogs had undulating surfaces, shallow pools and lateral seepages.

Outcome
undulating surfaces, large shallow pools, and lateral seepagese0
Setting
ridge-shaped raised bogse0

Not reportedTaxon

Verbatim

e0

“Distinctive features of the ridge-shaped raised bogs are their undulating surfaces, large shallow pools, and lateral seepages”

✓ located verbatim in the source · abstract, characters 226–351 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Bog vegetation was acidophilous and low in pH except where fen plants or patches occurred.

Taxon
Bog vegetatione0
Outcome
acidophilous and low in pH valuee0
Qualifier
except in limited arease0

Verbatim

e0

“Bog vegetation, typical of ombrotrophic peatlands, is acidophilous and low in pH value except in limited areas, e.g. fissures caused by frost heaving where fen plants are found, also the lateral seepages where patches of true fen vegetation appear along the rows of flarks.”

✓ located verbatim in the source · abstract, characters 435–708 · show in text ↑
Associationobservedoriginal resultmeasured

Claim · model-written summary

Bog plant communities were almost identical to those of raised bogs in Sweden and Finland.

Taxon
plant communitiese0
Outcome
almost identicale0
Comparator
similar raised bogs in Sweden and Finlande0

Not reportedDirection

Verbatim

e0

“The plant communities are almost identical with those of similar raised bogs in Sweden and Finland.”

✓ located verbatim in the source · abstract, characters 709–808 · show in text ↑
Associationobservedoriginal resultmeasured

Claim · model-written summary

Fen vegetation was richer in mineral nutrients than bog vegetation and resembled Scandinavian rich fen vegetation.

Taxon
vegetatione0
Outcome
vegetation richer in mineral nutrientse0
Direction
richere0
Comparator
that of the bogse0
Setting
Scandinaviae0

Verbatim

e0

“The fen water is highly minerotrophic, resulting in vegetation richer in mineral nutrients than that of the bogs, and similar to the "rich fen" or "brown fen" vegetation of Scandinavia.”

✓ located verbatim in the source · abstract, characters 900–1085 · show in text ↑
Observationobservedoriginal resultmeasured

Claim · model-written summary

Black-spruce islands in fens had permafrost cores.

Taxon
black-sprucePicea marianae0
Outcome
permafrost corese0
Setting
fene0

Organisms pictured · Representative pictures of the matched species, not figures from the paper.

Picea mariana
Picea mariana · TaxonLBM1948 · CC BY-SA 4.0 · Wikimedia Commons ↗

Verbatim

e0

“Roundish "black-spruce islands" are conspicuous fen features; they have permafrost cores”

✓ located verbatim in the source · abstract, characters 1086–1174 · show in text ↑