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Contributions to the Study of Biological Diversity Vol. 3<br />

(FCC) scene was composed <strong>in</strong> ArcView 3.3<br />

(ESRI 2002), us<strong>in</strong>g b<strong>and</strong> 2 (green, 0.53 - 0.61<br />

:m), b<strong>and</strong> 3 (red, 0.63-0.69 :m), <strong>and</strong> b<strong>and</strong> 4<br />

(near-<strong>in</strong>frared, 0.78-0.90 :m) (Figure 1.9, <strong>in</strong><br />

grayscale).<br />

Japanese Earth Resources Satellite (JERS-<br />

1) Synthetic Aperture Radar images from<br />

October 1995 were obta<strong>in</strong>ed from the Global<br />

Ra<strong>in</strong> Forest Mapp<strong>in</strong>g Project (2001). The image<br />

was registered <strong>in</strong> ArcView by creation of a<br />

‘world file’ (ESRI 2002) with coord<strong>in</strong>ates of the<br />

po<strong>in</strong>t of orig<strong>in</strong> <strong>and</strong> the fraction of a degree<br />

represented by one pixel on each axis. Features<br />

visible <strong>in</strong> the JERS image (Figure 1.10) served<br />

as an additional guide for del<strong>in</strong>eation of preburn<br />

plant community boundaries.<br />

Figure 1.10. JERS-1 radar image of the entire Wa<strong>in</strong>i<br />

Pen<strong>in</strong>sula, acquired <strong>in</strong> October 1995, resolution 3 arcseconds,<br />

about 95 meters at the latitude of this image.<br />

On the coastal pla<strong>in</strong>, dark areas primarily represent<br />

open water <strong>and</strong> smooth moist surfaces, while areas<br />

of high return represent dist<strong>in</strong>ct settlements or areas<br />

of flooded, <strong>in</strong>tact forest, which is the likely<br />

<strong>in</strong>terpretation along the coast near the right side of<br />

the image. Hills are visible along the center of the<br />

left edge, near the Northwest District=s adm<strong>in</strong>istrative<br />

seat, Mabaruma.<br />

Ground-truth transects were made across<br />

the Wa<strong>in</strong>i Pen<strong>in</strong>sula <strong>in</strong> <strong>and</strong> near the Almond<br />

Beach burn <strong>in</strong> April <strong>and</strong> October 2001. Two<br />

transects were made through central parts of the<br />

burn, <strong>and</strong> two others were made near each end<br />

of the burn (Figure 1.11). Transects were spaced<br />

approximately 2.5 to 3.5 km apart. Transect A<br />

crossed the Pen<strong>in</strong>sula near its northwestern end,<br />

<strong>in</strong> unburned forest. Transect B was made from<br />

the vic<strong>in</strong>ity of Almond Beach camp across<br />

19<br />

burned swampl<strong>and</strong>. Transect C started just east<br />

of the Almond Beach school, cross<strong>in</strong>g burned<br />

swampl<strong>and</strong> <strong>and</strong> <strong>in</strong>tact forest near the Wa<strong>in</strong>i<br />

River. Transect D was <strong>in</strong>tended to pass beyond<br />

the southeastern end the Almond Beach burn,<br />

however was adapted <strong>in</strong> the field to co<strong>in</strong>cide<br />

with a boundary of the burn. Transect E was a<br />

shorter exploration made beyond the<br />

southeastern limit of the Almond Beach burn.<br />

Along the transects at localities with<br />

dist<strong>in</strong>ctive vegetation types, vegetation<br />

transitions, burn boundaries, or plant collection<br />

localities, coord<strong>in</strong>ates were recorded us<strong>in</strong>g a<br />

GPS receiver, plant species at those locations<br />

were noted. Voucher specimens were collected<br />

wherever a species was previously uncollected<br />

or field identification was uncerta<strong>in</strong>. Transects<br />

B <strong>and</strong> C were each traversed twice, due to the<br />

time required to <strong>in</strong>itially clear or mark routes.<br />

A post-burn profile was composed to<br />

provide a visual representation of plant<br />

communities across the Almond Beach burn at<br />

transect C. The first tropical forest survey<br />

utiliz<strong>in</strong>g profiles was apparently performed <strong>in</strong><br />

Guyana (at that time British Guiana) by Davis<br />

<strong>and</strong> Richards (1933), detail<strong>in</strong>g a mixed lowl<strong>and</strong><br />

forest on Moraballi Creek near the Essequibo<br />

River; for that study all trees along a narrow<br />

transect were cut <strong>and</strong> measured as the profile<br />

was drawn. While Ellison (2002) argued that<br />

mangrove community profiles are subjective<br />

representations of structure <strong>and</strong> zonation unless<br />

they are l<strong>in</strong>ked to quantitative data, generalized<br />

Figure 1.11. Positions of transects across the Almond<br />

Beach burn (B, C, D) <strong>and</strong> outside of the burn (A, E)<br />

on the Wa<strong>in</strong>i Pen<strong>in</strong>sula. Po<strong>in</strong>ts <strong>in</strong>dicate locations of<br />

GPS read<strong>in</strong>gs where plant community <strong>in</strong>formation<br />

was gathered.

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