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Lake Panasoffkee SWIM Plan - Southwest Florida Water ...

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plant management effort targets<br />

exotic species. Some limited<br />

tussock removal has been done<br />

when navigation channels were<br />

blocked.<br />

<strong>Lake</strong> Sediments<br />

In 1957, <strong>Lake</strong> <strong>Panasoffkee</strong><br />

sediments were reported to consist<br />

predominantly of "deep, fine<br />

yellowish inorganic silt underlain by<br />

sand, blue clay and limestone*<br />

(Moody 1957). Deep black organic<br />

muck was found over sand. silt and<br />

soft limerock near the lake shore.<br />

There is concern that the lake is<br />

becoming increasingly shallow. It<br />

had been suggested that this could<br />

be due to sediment accumulation<br />

and that this is the principal<br />

ecological problem of the lake<br />

(Greiner 1978).<br />

.<br />

Sediment<br />

Thickness<br />

/<br />

5 - 10 feet<br />

00 - 20 feet.<br />

Greiner (1978) stated that lake<br />

sediments consisted principally of<br />

precipitated limestone rather than<br />

organic deposits. This report also igure A-3. Sediment thickness map after Belanger et al. 1993<br />

concluded that lake depths in the<br />

south end of the lake had been decreased by sediments eroding off of uplands and carried<br />

to the lake by Shady Brook. Brenner and Binford (1988) sampled mid-lake sediments in <strong>Lake</strong><br />

- <strong>Panasoffkee</strong> and found that surface sediments had the highest carbonate content out of 97<br />

<strong>Florida</strong>n lakes sampled which indicates that the sediments are largely inorganic; however,<br />

these were mid-lake readings, and no samples were taken from the shallower near-shore<br />

areas.<br />

A <strong>SWIM</strong>-funded project, performed by the <strong>Florida</strong> Institute of Technology (Belanger et al.<br />

1993). investigated sediment composition and distribution in <strong>Lake</strong> <strong>Panasoffkee</strong>. Belanger et<br />

al. (1993) determined that sediments in <strong>Lake</strong> <strong>Panasoffkee</strong> contain much more inomanic<br />

carbonate matter (72.3 percent) than organic matter (17.4 percent). he study focused on the<br />

~0Ssible causes of the increasina shallowness. the sources of sediment. and the extent of<br />

knmade versus natural lakedegradation. ~edihents were mapped by depth-to-hardpan and<br />

analyzed according to physical and chemical characteristics. Belangeret al. (1993) employed<br />

PB-210 dating, organic matter "biomarker" and paleolimnology analysis to assist the<br />

investigation.

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