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The ecology of eelgrass meadows in the Pacific Northwest: A ...

The ecology of eelgrass meadows in the Pacific Northwest: A ...

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storms erode and dislodge some <strong>eelgrass</strong>,<br />

but most is very persistent (~igure 2).<br />

Gallagher et al. (In prep.), however,<br />

found that ~eriodic storms do dislodge a<br />

large amount <strong>of</strong> eelyrass <strong>in</strong> w<strong>in</strong>ter and<br />

summer and deposit <strong>the</strong> material <strong>in</strong><br />

adjacent marshes <strong>in</strong> Netarts Bay, Oregon.<br />

<strong>The</strong> <strong>eelgrass</strong> litter constituted between<br />

14% and 35% <strong>of</strong> <strong>the</strong> dead material <strong>in</strong> <strong>the</strong><br />

marshes. <strong>The</strong>ir conclusion is that <strong>in</strong><br />

estuaries where seagrass beds ad jo<strong>in</strong><br />

marshes, <strong>the</strong> trapp<strong>in</strong>g <strong>of</strong> <strong>eelgrass</strong> litter<br />

<strong>in</strong> <strong>the</strong> marsh provides a mechanism for<br />

reta<strong>in</strong><strong>in</strong>g and recycl<strong>in</strong>g nutrients with<strong>in</strong><br />

<strong>the</strong> wetlands and prevent<strong>in</strong>g <strong>the</strong>ir loss to<br />

<strong>the</strong> oceanic system. <strong>The</strong>se nutrients )nay<br />

be passed back and forth between <strong>the</strong><br />

<strong>eelgrass</strong> and marsh systems. Also, <strong>in</strong><br />

Netarts Bay, Kentula (1983) calculated a<br />

total annual leaf loss which varied from<br />

25 to 111 g dry wt/m2. While <strong>the</strong> belowground<br />

biomass was reta<strong>in</strong>ed with<strong>in</strong> <strong>the</strong><br />

meadow, she observed that some <strong>of</strong> <strong>the</strong><br />

;Iboveground biomass was carried shoreward<br />

and trapped by <strong>the</strong> salt marsh and some was<br />

transported out <strong>of</strong> <strong>the</strong> estuary. <strong>The</strong><br />

presence <strong>of</strong> <strong>eelgrass</strong> material <strong>in</strong> cores<br />

taken <strong>in</strong> Oregon salt marsh sediments<br />

implied <strong>the</strong> net transport <strong>of</strong> <strong>eelgrass</strong><br />

(Jefferson 1975).<br />

Probably normal Leaf defoliation and<br />

replacement is <strong>the</strong> source <strong>of</strong> most <strong>of</strong> <strong>the</strong><br />

detached leaf material observed <strong>in</strong> <strong>the</strong><br />

<strong>Pacific</strong> <strong>Northwest</strong>. Short (1975) estimated<br />

that <strong>eelgrass</strong> experienceda70% seasonal<br />

defoliation rate. Proctor et al. (1980b)<br />

used. this number and based on stand<strong>in</strong>gcrop<br />

estynates from Phillips (1974; 580 g<br />

dry wt/m , 260 tons/acre) and o<strong>the</strong>rs, to<br />

calculate that <strong>eelgrass</strong> <strong>meadows</strong> <strong>in</strong> <strong>the</strong><br />

<strong>Pacific</strong> <strong>Northwest</strong> produce annually about<br />

30,000 kg (66,0(110 tons, dry matter) <strong>of</strong><br />

<strong>eelgrass</strong> leaf material, <strong>of</strong> which 20,909 kg<br />

(46,000 tons) dry weight is defoliated<br />

annually to become detritus: 8,400 ha<br />

(21,000 acres) <strong>of</strong> <strong>eelgrass</strong> <strong>in</strong> Wash<strong>in</strong>gton;<br />

2,000 ha (5,BBB acres) <strong>in</strong> Oregon; and<br />

1,600 ha (4,000 acres) <strong>in</strong> nor<strong>the</strong>rn<br />

California.<br />

<strong>The</strong> only record <strong>of</strong> <strong>eelgrass</strong> blades <strong>in</strong> <strong>the</strong><br />

deep sea was made by Pearcy and Ambler<br />

(1974) who found <strong>the</strong> material as<br />

accidental contents <strong>in</strong> <strong>the</strong> abyssal<br />

rattail, Coqphaenoides armatus. -<br />

In <strong>the</strong> Carribbean, tropical seagrasses are<br />

exported and found at great depths<br />

(reviewed by Zieman 1982). At St. Croix,<br />

U.S. Virg<strong>in</strong> islands, 60%-1B0% <strong>of</strong> <strong>the</strong><br />

Syr<strong>in</strong>gcdium f ilifonne daily production was<br />

detached and exported, whereas only 1% <strong>of</strong><br />

<strong>the</strong> Thalassia production was exported by<br />

bedload transport (Zieman et al. 1979).<br />

Leaves and rhizome pieces <strong>of</strong> ~halassia<br />

were collected <strong>in</strong> 3,160 m (10,368 ft) <strong>of</strong><br />

water <strong>of</strong>f North Carol<strong>in</strong>a (Menzies et dl.<br />

1967); at 3,580 m (11,484 ft) deep <strong>of</strong>f <strong>the</strong><br />

Virg<strong>in</strong> Islands (Raper and Brundage 1972);<br />

and from 1,326-8,339 rn (4,376-27,489 ft)<br />

deep <strong>in</strong> <strong>the</strong> Puerto Rican and Cayman<br />

trenches (Wolff 1988). Wolff reported<br />

consumption <strong>of</strong> <strong>the</strong> leaf and rhizome<br />

material by numerous <strong>in</strong>vertebrates.<br />

F<strong>in</strong>ally, <strong>the</strong> important mechanis~n that<br />

leads to detritus production and ei<strong>the</strong>r<br />

entrapment or export from <strong>the</strong> seagrass<br />

system is <strong>the</strong> decomposition and<br />

<strong>in</strong><strong>in</strong>eralization <strong>of</strong> <strong>the</strong> Leaf material that<br />

becomes detached frorn <strong>the</strong> plants. Only<br />

two field studles have been conducted on<br />

seagrass leaf decay rates (litter bay<br />

analyses): one on Thalassia (~iemdn 1968)<br />

,md om on <strong>eelgrass</strong> (Burkholder and D<strong>of</strong>wny<br />

1968). Two studies were conducted <strong>in</strong> <strong>the</strong><br />

laboratory (~arrison and Mann 1975a;<br />

Wshalk and Wetzel 1978). Zieman (L%8)<br />

observedthat Thalasei* leaves <strong>in</strong> litter<br />

bags anchored <strong>in</strong> areas subject to<br />

alternat<strong>in</strong>g perids <strong>of</strong> dry<strong>in</strong>g and wett<strong>in</strong>g<br />

lost weight three times as fast as those<br />

<strong>in</strong>cubated <strong>in</strong> tanks where <strong>the</strong>y were<br />

constantly wet. Predried ~ hal ass ia leaves<br />

nlaced <strong>in</strong> tanks lost weiqht five tirnes<br />

;aster than leaves not predried. Dry<strong>in</strong>g<br />

is considered to destroy <strong>the</strong> cellular<br />

<strong>in</strong>tegrity more rapidly and allow a more<br />

rapid microbial attack. Zieman also found<br />

a 50% weight loss <strong>of</strong> leaves after 5 wk <strong>of</strong><br />

<strong>in</strong>cubation <strong>in</strong> tanks <strong>of</strong> circulat<strong>in</strong>q<br />

10% loss was<br />

~n ~ ~ Carol<strong>in</strong>a, ~ t mayer h et al. (1979) seawater. Only an additio~l<br />

reported that up to 25% <strong>of</strong> <strong>the</strong> production Observd <strong>the</strong> next wk*<br />

<strong>in</strong>- open water-beds is exported to <strong>the</strong><br />

adjacent estuary, while <strong>in</strong> embayment-type In New York Burkholder and Doheny<br />

beds over 90% <strong>of</strong> <strong>the</strong> production decays <strong>in</strong> (1968) placed fresh eelyrass leaves <strong>in</strong><br />

<strong>the</strong> bed or is washed up onto adjacent litter bags <strong>in</strong> two locations. At one site<br />

beaches and marshes. only 23% <strong>of</strong> <strong>the</strong> material rema<strong>in</strong>ed after 56

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