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(Stachys: Lamiaceae) from the - Botanical Research Institute of Texas

(Stachys: Lamiaceae) from the - Botanical Research Institute of Texas

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Fleming et al., A new species <strong>of</strong> <strong>Stachys</strong> <strong>from</strong> <strong>the</strong> sou<strong>the</strong>astern United States 13<br />

Fig. 4. County distribution <strong>of</strong> <strong>Stachys</strong> mat<strong>the</strong>wsii specimens in Virginia and North Carolina.<br />

competitive with taller, ruderal perennials. Plants growing in a formerly cleared floodplain now invaded by<br />

young trees have become progressively shade-stressed and do not flower. A periodically mowed powerline<br />

swale with short to medium-height herbaceous vegetation appears to represent optimal habitat for <strong>the</strong> species,<br />

supporting a population with hundreds <strong>of</strong> flowering plants. Perhaps <strong>the</strong> combination <strong>of</strong> shade-intolerance<br />

and poor competitive abilities, as well as low levels <strong>of</strong> botanical inventory in <strong>the</strong> Piedmont, accounts for <strong>the</strong><br />

relatively low number <strong>of</strong> known populations, despite an abundance <strong>of</strong> seemingly suitable habitat in <strong>the</strong> region.<br />

Notes on <strong>the</strong> Distribution <strong>of</strong> <strong>Stachys</strong> mat<strong>the</strong>wsii<br />

<strong>the</strong>re is precedence for <strong>the</strong> somewhat disjunct distribution <strong>of</strong> populations <strong>of</strong> stachys mat<strong>the</strong>wsii between <strong>the</strong><br />

north carolina - Virginia Piedmont and calcareous habitats <strong>of</strong> <strong>the</strong> Virginia coastal Plain. Previous investigations<br />

by ware and ware (1992) and macdonald (2000) point to numerous species <strong>of</strong> primarily Piedmont<br />

and mountain distribution with outlying populations in or adjacent to coastal ravine complexes underlain<br />

by <strong>the</strong> calcareous Yorktown and eastover formations. <strong>the</strong>se Pliocene deposits, due to <strong>the</strong>ir highly erodible<br />

nature, have allowed for <strong>the</strong> creation <strong>of</strong> relatively dramatic ravine complexes within <strong>the</strong> o<strong>the</strong>rwise slightly<br />

undulating and acidic landscape <strong>of</strong> <strong>the</strong> tidewater region. it is widely assumed that <strong>the</strong> disjuncts present in<br />

or near such ravines are relics <strong>of</strong> early holocene climates, when species now confined to montane habitats<br />

were more broadly distributed in Virginia (delcourt & delcourt 1986). while stachys mat<strong>the</strong>wsii is not confined<br />

to <strong>the</strong>se steep - sided erosional features, <strong>the</strong> presence <strong>of</strong> populations immediately adjacent to <strong>the</strong>m<br />

on shelly substrates (and nowhere else in <strong>the</strong> region) certainly points to relictual distribution as a possible<br />

factor involved in <strong>the</strong>ir presence.

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