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BEN # 220



BBBBB    EEEEEE   NN   N             ISSN 1188-603X
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BBBBB    EEEEE    NN N N             BOTANICAL
BB   B   EE       NN  NN             ELECTRONIC
BBBBB    EEEEEE   NN   N             NEWS

No. 220                              April 7, 1999

aceska@freenet.victoria.bc.ca        Victoria, B.C.
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 Dr. A. Ceska, P.O.Box 8546, Victoria, B.C. Canada V8W 3S2
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PLANT DIVERSITY IN BARKLEY SOUND [Part 1 of 3]
From: Martin L. Cody <mlcody@ucla.edu>

THE TOPOGRAPHICAL AND HISTORICAL SCENE

About  one-third  of  the  way  up  the outer coast of Vancouver
Island, British Columbia, Barkley Sound is a 35 km2  indentation
dotted  with  hundreds of tiny to moderately-sized islands, with
several of the larger over 1 km2  in  area.  The  most  isolated
islands  comprise  the  Broken Group in the center of the Sound,
and are up to about 20 km from "mainland" Vancouver Island.  All
are  continental  or  landbridge  islands, representing hilltops
isolated with rising late-Pleistocene  sea-levels  (e.g.  Dawson
1992);  from marine charts showing channel depths, the oldest of
the present-day islands date from ca. 12,000 yBP, although  many
(with  shallow channel depths of a few meters) are much younger.
Very low-lying islands will have re-emerged relatively recently,
as continued coastal uplift has dropped relative sea level  3-4m
from  maximum  rise some 6-7,000 yBP (Friele & Hutchinson 1993).
Island substrates are uniformly rocky, composed  of  mixed  Ter-
tiary  volcanics  and  metamorphics  (Muller 1983, Yorath 1995);
their shores generally rocky, often steep, with a few sandy  and
many mud/cobble beaches. Most islands are in pristine condition;
those  in the Broken Group are part of Pacific Rim National Park
and  several  support  camping  beaches;  others  are  variously
private,  First  Nations, or Crown land. Being exposed and rela-
tively low-lying, the islands are  generally  dry  with  shallow
soils,  and fresh water seeps reaching the beach only on islands
>105 m2 in area. The climate (at Bamfield, s. edge of the Sound)
is wet maritime, ave. 2950 mm of precipitation/y, but  only  ca.
10%  of  the  annual total falls in the three summer months Jun-
Aug.

Diversity, distribution, dispersal and  population  dynamics  of
plant  species in from forest to shoreline have been the subject
of biogeographic and ecological studies since 1981.  Plant  sur-
veys on islands in Barkley Sound have continued up to 1997, with
ten summer seasons spent in the area (Cody 1992a,b, 1998; Cody &
Overton  1996).  To  date,  some 210 islands have been surveyed,
many of these  repeatedly,  often  in  adjacent  or  subadjacent
years.  Surveyed islands cover a size range of about 6 orders of
magnitude, and the largest samples sizes are in the  range  102-
104  m2;  nearly  40% of the sample islands are in the center of
the Sound, the  remainder  closer  to  the  mainland  (Vancouver
Island)  coast. All surveyed islands have been accurately mapped
by transit at the Fucus line and by elevational contours  at  1,
2,  5,  10,  20  and  50 m intervals, with coverage of the major
vegetation types superimposed.

THE FLORA: VEGETATION, DIVERSITY AND DISTRIBUTION

The vegetation of the mainland coastal areas and  over  much  of
the  larger  islands is Coastal Coniferous Forest (Klinka et al.
1989, Pojar & MacKinnon 1994; for floristics, I follow Hitchcock
& Cronquist 1973). The forests are dominated by Red Cedar (Thuja
plicata), Sitka Spruce (Picea sitchensis), and  Western  Hemlock
(Tsuga  heterophylla),  with  occasional firs (Abies grandis, A.
amabilis), alders (Alnus rubra), and maples (Acer  macrophyllum,
A.  douglasii).  On  the islands (only) Douglas fir (Pseudotsuga
menziesii) is common, coast pines (Pinus contorta) are found  on
all  shorelines,  with  Western White pine (P. monticola) on the
edges of bogs. The  forest  understory  is  composed  of  mostly
ericaceous shrubs such as Arctostaphylos, Gaultheria, Menziesia,
and  Vaccinium species, ferns, and a few geophytes (Maianthemum,
Goodyera, Listera) and forbs (Tiarella,  Boykinia).  Around  the
interior  forests on islands are concentric rings of first woody
shrubs (many Rosaceae, some Caprifoliaceae), second  a  zone  of
largely  weedy  herbaceous,  mostly  perennial  forbs  of a wide
variety of taxonomic  affinities  (especially  Asteraceae,  some
Brassicaceae,  Onagraceae,  Fabaceae),  and  lastly  a shoreline
flora of plants specific to rocky  shores  or  sandy,  muddy  or
cobble beaches, many of cosmopolitan distribution.

The  flora  of  the  islands is essentially that of the adjacent
mainland, since most habitats, even coastal marsh fragments  and
tiny  island  bogs,  are represented; it currently totals around
300 plant species. Some adjacent mainland species are absent  on
the  islands,  mostly  wetland species typical of shallow inlets
(e.g. Jaumea carnosa, Lilaeopsis occidentalis), extensive  sandy
beaches (Franseria chamissonis, Carex macrocephala), larger bogs
(e.g.  Vaccinium alaskense, V. uliginosum, Botrychium sp.), many
other freshwater aquatics  (e.g.  Lysichiton  americanum,  Carex
spp.),  and weedy plants, often aliens, typical of roadsides and
settlements (e.g. Senecio vulgaris, Medicago, Vicia  spp.  among
others).

But the islands support additional plant species that are rarely
or  never  seen  on  the  immediately adjacent mainland, such as
Douglas-fir, manzanita (Arctostaphylos  columbianum)  and  other
plants  more  typical  of the inner and drier (NE) coast of Van-
couver Island, and  additionally  various  shoreline,  rock  and
cliff  plants  (e.g.  Baeria  maritima,  Cochlearia officinalis,
Carex  pansa).  Other  notable  island  records  include   Carex
gmelinii,  present  on  a single cluster of islands at the outer
edge of the Sound.

The largest islands  support  around  125  plant  species,  with
species numbers declining with area in the classical manner. The
larger  islands in Barkley Sound (logA[rea] > 4.25) fit the same
regression line:

logSPP = 0.661 + 0.241*logA (r**2 = 0.764, p <.001), 

regardless of isolation.  This would indicate that their species 
numbers (and composition) reflect a pre-isolation state  typical
of supersaturated non-equilibrial  landbridge  islands,  largely
uninfluenced by colonization. Variation in  species  composition
among these islands suggests two lines of enquiry:

 1. some  species  persist  only on less isolated islands, where
    they  may  be  retained  by  a  rescue  effect  via  ongoing
    colonization;

 2. some  species  occur  on island groups by dint of historical
    legacy. For example, two plant species, Carex  gmelinii  and
    Streptopus  amplexifolius,  have  been  found  on just three
    islands, mutual neighbors in  the  Deer  Group  which  (from
    channel  depths)  have  shared a common branch of the island
    "phylogeny" for ca. 10,000 y.

Joint occurrence of species on islands for  reasons  independent
of  similar  area (incidence) have been systematically evaluated
for rescue and historical legacy influences.

On the other hand, small-island groups have species-area  curves
that  differ  as  a  function  of isolation distance, with lower
species numbers on more distant islands;  their  differences  in
diversity,  per  area, are attributable therefore to differences
in the rates of on-going colonization.
[Continuation in BEN # 221]


RE: PROMINENT BOTANIST-BRYOLOGIST COURT-MARTIALED

[Benito Tan, a BEN subscriber, posted my  note  about  Archibald
Menzies  on  the  bryological  discussion  list  BRYONET-L. This
posting triggered an interesting discussion on the role  of  Dr.
Archibald  Menzies  as  a  bryologist.  I  am  using two replies
originally posted on BRYONET-L. - AC]

From: David Long <D.Long@rbge.org.uk>

In Edinburgh we have Menzies' own cryptogamic herbarium which is
one of the most meticulously prepared collections I  have  seen.
He was clearly an extremely eagle-eyed and careful collector and
searched  hard  for  sporophytes  in  the field, and most of his
liverworts bear sporophytes. Of course  he  sent  duplicates  to
William  Hooker  in Glasgow who published most of the novelties;
these holotypes are now in BM (ex K), but the isotypes  he  kept
in  his  own  herbarium are in pristine condition and one of our
most prized assets in Edinburgh. The specimens  are  mounted  on
small  sheets with the data (scanty but usually with place, year
and 'AM') on the reverse. Menzies also received many  duplicates
from  James Dickson, Swartz, Schleicher, Schwaegrichen and other
contemporaries and was not just a good collector but  a  serious
student of cryptogams.

Further information on Archibald Menzies is to be found in:

Balfour,  F.R.S.  1945. Archibald Menzies 1754-1842. Proc. Linn.
   Soc. London 156: 170-183.
Haber, E. 1985. The type locality  for  Menzies'  collection  of
   Pyrola  picta,  P. dentata, and P. aphylla from the northwest
   coast of North America. Taxon 34: 462-463.
Galloway, D.J. & E.W. Groves. 1987. Archibald  Menzies  MD,  FLS
   (1754-1842),  aspects  of  his life, travels and collections.
   Archives of Nat. Hist 14: 3-43.
Naish, J. 1989. Archibald Menzies: Surgeon  and  Botanist.  Int.
   Dendrol. Soc. Year Book 1988: 123-128.


From: Allan Fife <FifeA@landcare.cri.nz>

There  are  two  other references that those with an interest in
Menzies might wish to consult:

Galloway, D.J. 1995. The extra-European  lichen  collections  of
   Archibald  Menzies,  M.D.  FLS (1754-1842). Edinb. J. Bot. 52
   (2): 95-139.
Godley, E.J. 1960. A note on Archibald Menzies. Trans. Roy  Soc.
   New Zealand 88: 63-64.


CORRECTION: SPRING GATHERING TO REMEMBER CHESS LYONS

The  spring  gathering  to  remember Chess Lyons (see BEN # 212)
will take place on Sunday, April 11, 1999 at Freeman King Nature
House, in GOLDSTREAM PROVINCIAL PARK from 2:00 to 4:00 p.m., NOT
in "Freeman-King Park," as previously stated.

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