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C4 grasses in boreal fens: their occurrence in relation to microsite characteristics

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Abstract

C4 plants are rare in cool climates, an ecological pattern attributable to their poor photosynthetic performance at low temperatures relative to C3 species. However, some C4 species are able to persist at high latitudes and high elevations, possibly due to the characteristics of the particular microsites they inhabit in these otherwise unfavourable environments. One such species is Muhlenbergia glomerata, which occurs above 60°N in Canada and is found in the atypical C4 habitat of boreal fens. In this study, we evaluate how microsite features affect the success of M. glomerata in boreal fens. We surveyed 19 populations across northern Ontario during the summers of 1999 and 2000. The ground coverage by woody vegetation was the most important parameter affecting the presence or absence of M. glomerata. Woody plants covered over 50% of the ground area in plots where M. glomerata is absent, but less than 20% where it is present. The minimum light intensity threshold for the presence of the C4 species was about 32% of full-sunlight at plant height. Surprisingly, in boreal fens M. glomerata was largely restricted to the wetter moss hollows, rather than occurring on the dry hummocks where its greater water use efficiency might have been advantageous. Woody species dominated the hummocks, but were uncommon in the hollows. In these cool northern climates M. glomerata apparently persists because sufficient periods of temperatures favourable to C4 photosynthesis occur, but this persistence likely requires some factor that suppresses the woody vegetation.

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Acknowledgements

The authors wish to thank Deb Metsger (TRT), Erika North (LKHD), Lada Malek (Lakehead) and Dan Paju (Thunder Bay) for access to herbarium collections, and to Barb and Garnie Sproule for access to the Mosque field site. We appreciate the helpful comments of two anonymous reviewers. This work was funded by an NSERC grant (OGP0154273) to R.F.S.

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Correspondence to David S. Kubien.

Appendix

Appendix

Details of the sites used to quantify the characteristics of the microsites which support populations of Muhlenbergia glomerata in Ontario

Populations were considered distinct when a hydrological discontinuity was apparent. Sites are typically named by the township in which they occur. Grid references follow the Universal Transverse Mercator (UTM) system, as indicated on the National Topographic System (NTS) of Canada map series (Natural Resources Canada 1999). Note that the populations on this list represent 19 out of over 200 fens examined for the presence of M. glomerata.

Year

Site

Latitude

Longitude

NTS map (1:50,000)

UTM grid reference

Day of year

1999

Batchawana

46 57

84 33

41 K/15

865 022

196

Pancake Bay

46 58

84 45

41 K/15

739 041

209

Pardee

48 08

89 35

52 A/4

070 358

201

Prairie River

48 48

86 47

42 D/15

157 055

206

T-Bay NW

48 24

89 18

52 A/6

265 644

202

T-Bay SW

48 23

89 20

52 A/6

271 640

203

Mosque

44 58

76 54

31 C/15

506 846

189

Clarendon

45 00

76 53

31 F/2

507 848

190

2000

Carmichael

49 05

82 00

42 G/1

267 371

185

Ford

49 02

82 02

42 G/1

248 323

186

McMillan

49 46

84 40

42 F/15

682 159

191

McCoig

49 45

84 49

42 F/15

572 146

192

Lindwest

49 43

87 08

42 E/11

904 063

193

Wildgoose

49 43

87 09

42 E/11

895 062

194

Errington

49 41

87 03

42 E/11

966 041

195

Stedman

49 05

90 41

52 G/2

690 389

197

Colliver

49 06

90 42

52 G/2

678 403

201

Fisher

46 56

84 33

41 K/15

862 051

208

Herrick

46 57

84 38

41 K/15

798 029

210

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Kubien, D.S., Sage, R.F. C4 grasses in boreal fens: their occurrence in relation to microsite characteristics. Oecologia 137, 330–337 (2003). https://doi.org/10.1007/s00442-003-1369-2

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