Seed bank, biomass, and productivity of Halophila decipiens, a deep water seagrass on the west Florida continental shelf
Introduction
One of the largest, open-water, contiguous seagrass ecosystems in the world occurs on the shallow continental shelf in the eastern Gulf of Mexico adjacent to the west coast of Florida, USA (CSA Inc., 1985, CSA Inc., 1987, CSA Inc., 1991; Iverson and Bittaker, 1986, Fourqurean et al., 2001). This area is referred to as the west Florida shelf (WFS) and extends from Cape San Blas south to Cape Sable and the Florida Keys (Fig. 1, inset). The WFS encompasses 75% of the total continental shelf area of the Gulf of Mexico and with its associated shallow water estuaries (<10 m water depth) it was estimated to contain approximately 9100 km2 of seagrass coverage or about 76% of the total coverage in the Gulf of Mexico (Iverson and Bittaker, 1986). On relatively deeper portions of the shelf, between 10 and 30 m, there is estimated to be an additional 20,000 km2 of seasonally ephemeral Halophila decipiens habitat interspersed with unvegetated soft sediments and diverse benthic communities of calcareous and fleshy macroalgae, crustacean burrows, and hard bottom outcrops dominated by sponges and soft corals (CSA Inc., 1985, CSA Inc., 1991Phillips et al., 1990, Fourqurean et al., 2001). The non-seagrass habitats harbor motile invertebrates and fishes that utilize adjacent H. decipiens meadows (Phillips et al., 1990). This region of the Gulf of Mexico supports some of the richest coastal fisheries in the United States (Mahmoudi et al., 2002). Depending on climatic conditions and severe storms, portions of this seagrass ecosystem may completely disappear from the shelf in winter, as is the case in other ephemeral seagrass populations (CSA Inc., 1987, CSA Inc., 1991Williams, 1988, Jupp et al., 1996, Kenworthy, 2000). Although shallow water seagrass populations have been well-studied, little is known about the demography, reproductive biology and life history mechanisms which maintain the deeper water seagrass ecosystems throughout the world (Kenworthy et al., 1989, Lee Long et al., 1996, Erftemeijer and Stapel, 1999).
H. decipiens occurs in tropical and sub-tropical seas worldwide (den Hartog, 1970, Waycott et al., 2002). It grows in many types of unconsolidated substrate, from soft, silty sediments to coarse shell hash, and is capable of stabilizing the seafloor (Fonseca, 1989). Like many of the larger taxa, H. decipiens provides a source of organic matter, habitat structure and food for benthic and pelagic organisms, including sea turtles and dugongs (Ross, 1985, Josselyn et al., 1986, Dirnberger and Kitting, 1988, Kenworthy et al., 1989, Lanyon et al., 1989, Preen, 1995, Russell et al., 2003). It is distributed from the shallow subtidal to depths of >40 m, where it forms extensive habitat in lagoons, on continental shelves, and in other deep water environments (den Hartog, 1970; CSA Inc., 1985, CSA Inc., 1991; Kenworthy et al., 1989, Lee Long et al., 1996, Fourqurean et al., 2001). As is the case for other members of the genus, H. decipiens is a ruderal species adapted to surviving in diminished and fluctuating light regimes and thrives in environments where disturbances such as herbivory, bioturbation, and storms make conditions unsuitable for maintaining perennial populations of the competitively superior, larger, and longer-lived seagrasses (Josselyn et al., 1986; Continental Shelf Associates, Inc., 1987; Williams, 1988, McMillan and Soong, 1989, Duarte, 1991, Kenworthy et al., 1993, Kuo and Kirkman, 1995, Preen, 1995, Jupp et al., 1996, Lee Long et al., 1996, Kenworthy, 2000).
H. decipiens is monecious and forms flowers and fruits at the base of the leaf pairs, at or just beneath the sediment surface. Seeds are negatively buoyant (McMillan, 1988a), and are thus ideally suited to percolate into the sediment. In laboratory settings, Halophila spp. seeds have germinated after 1–2 years of storage under dark conditions (McMillan, 1991, McMillan and Soong, 1989), suggesting that members of this genus could rely on a buried seed bank to re-establish populations. Although H. decipiens may propagate vegetatively by fragmentation (Hall, 2002), annual populations likely reestablish through germination of seeds maintained in a persistent sediment seed bank. This hypothesis is suggested by observations of ephemeral H. decipiens populations in Florida, the Virgin Islands, Panama, and Australia (Williams, 1988, McMillan and Soong, 1989; Continental Shelf Associates, Inc., 1991; Kuo and Kirkman, 1995, Kuo et al., 1995, Kenworthy, 2000). Seed banks are a valuable trait for recruitment of plants living in seasonally fluctuating environments or unpredictable habitats where disturbance is common (McMillan and Soong, 1989, Fenner, 1995, Inglis, 2000a, Kenworthy, 2000), typical growing conditions for H. decipiens.
Although several descriptive studies and many independent observations have corroborated the seasonality of the large west Florida shelf seagrass ecosystem, no one has yet examined the demography and reproductive ecology of H. decipiens and the specific mechanisms that result in persistent deep water (10–20 m) populations. The objective of this paper is to quantify and describe H. decipiens biomass, productivity and reproductive ecology along a depth gradient transect in the southern region of the west Florida shelf, extending from the shallowest to deepest ranges of the plants’ distribution. Specifically, we examine variability in the sediment seed bank, seedling density, flowering, fruiting, productivity and biomass to gain a better understanding of the mechanisms controlling the distribution and abundance of this widely dispersed species.
Section snippets
Study site
Samples were collected along an onshore to offshore transect on the WFS during June, August, and October 1999 and January and July 2000 cruises. This transect was centrally located within the southeastern region of the WFS where two previous overlapping benthic community surveys spanning multiple years documented the widespread, persistent distribution of H. decipiens (Fig. 1) (Continental Shelf Associates, Inc., 1991; Fourqurean et al., 2001). In June 1999 we established three permanent 1 km × 1
Seagrass biomass and reproduction
To examine patterns of spatial and temporal variability, three level nested analysis of variance was used to test the effect of date, station nested within date, and quadrat nested within station on biomass and reproductive parameters. Data were log transformed (leaf pair, apical, flower, fruit, and seedling density) or square-root transformed (biomass) to meet assumptions of normality and variance homogeneity. Analysis of variance is robust to departures from normality and variance
Site characteristics
Extinction coefficients, light penetration and daily PAR were generally highest at the nearshore station and lowest at the offshore station (Table 1). Percent surface irradiance ranged from 6.3 to 22.4%, while daily PAR ranged from 1.8 to 7.1 mol m−2 day−1. Although % SI and daily bottom PAR varied across stations and cruise dates, the only notable change occurred during October 1999, when Hurricane Irene passed directly over the field site and caused a 97% decline in daily PAR at the bottom.
Seagrass cover, biomass and productivity
The percent cover of H. decipiens was typical for Halophila spp. and similar to studies in this region of the WFS (Continental Shelf Associates, Inc., 1991; Fourqurean et al., 2001, Kenworthy, 2000). Our depth transect was centered in two previous, spatially overlapping benthic surveys so that our process-oriented study of growth and reproduction at the three different depths could be inferred over a wider geographic distribution (Fig. 1). Cover was patchy throughout the study area, tended to
Acknowledgements
Our thanks to M. Alanen, D. Berns, C. Bonn, R. Conroy, R. Dean, P. Hall, J. Hyniova, M. Merello, J. Parker and the crews of the NOAA ships FERREL and OREGON II and the USF ship R/V Suncoaster for help with sample collection and processing. Reviews by G. Inglis, P. Marraro, J. Vermaat, M. Waycott, and two anonymous reviewers improved this manuscript. Funding was provided by NOAA's National Marine Sanctuary Program, the Center for Coastal Fisheries and Habitat Research, Beaufort, NC, and the
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Present address: Moss Landing Marine Laboratories, 8272 Moss Landing Road, Moss Landing, CA 93933, USA.