Bryophytes of springs and flushes - 2009 course notes - Plantlife
Bryophytes of springs and flushes - 2009 course notes - Plantlife
Bryophytes of springs and flushes - 2009 course notes - Plantlife
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Philonotis calcarea) to moderately acidic. The common feature is the <strong>of</strong>ten extensive mats <strong>of</strong><br />
Philonotis fontana usually with a mix <strong>of</strong> other bryophytes including Dichodontium palustris,<br />
Brachythecium rivulare, Bryum pseudotriquetrum, Scapania undulata <strong>and</strong> on the margins<br />
Sphagnum denticulatum. Higher st<strong>and</strong>s may also have Bryum weigelii (the pink in the flush<br />
above bottom right), Philonotis seriata <strong>and</strong> Scapania uliginosa (above bottom left). Lower<br />
down many flushed areas have st<strong>and</strong>s <strong>of</strong> Philonotis fontana, <strong>of</strong>ten with the typical associates<br />
but the vascular plant component is usually different, <strong>of</strong>ten Montia fontana or<br />
Chrysosplenium oppositifolium.<br />
M33 Pohlia wahlenbergii var. glacialis spring<br />
This is the arctic-montane equivalent <strong>of</strong> the<br />
M32 flush characterised by large pure st<strong>and</strong>s<br />
<strong>of</strong> Pohlia wahlenbergii var. glacialis, which<br />
are <strong>of</strong>ten visible from some distance.<br />
Associated bryophyte species are <strong>of</strong>ten<br />
limited but include Philonotis fontana, Pohlia<br />
ludwigii, Scapania uliginosa, Scapania<br />
undulata <strong>and</strong> Marsupella sphacelata.<br />
M37 Palustriella commutata – Festuca rubra spring <strong>and</strong> M38 Palustriella commutata –<br />
Carex nigra spring<br />
These are the ‘brown moss’ <strong>springs</strong> characterised by large st<strong>and</strong>s <strong>of</strong> Palustriella commutata<br />
or Palustriella falcata, <strong>of</strong>ten to the exclusion <strong>of</strong> other bryophytes. They <strong>of</strong>ten occur as small<br />
patches at the spring-head <strong>of</strong> other calcareous flush types but in limestone areas can form<br />
extensive st<strong>and</strong>s <strong>of</strong>ten with some tufa formation.<br />
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