MARINE MEADOW AND SURFWEED COMMUNITIES

Most people, in fact, most biologists, are unaware that there are two submarine, totally submerged habitats for flowering plants, i.e., hidden beneath the waves, along tropical and temperate coastlines, where one expects to find only marine algae. The habitats are called marine meadow and surfweed. The surfweed community is more commonly known as kelp forest. Both habitats and three species of special seed-bearing halophytes occur submerged below tide along the California coastline.

In all, 58 species of monocotyledons, collectively termed seagrasses or marine phanerogams, live in such habitats, especially in marine meadows, where they are the primary producers of, probably, the most productive community on Earth. Marine meadows are especially famous as the feeding grounds of grazing, herbivorous dugongs and sea turtles, which is why certain species are called turtlegrass.

Seagrasses thrive in shallow sedimentary environments of mainly warm tropical waters, especially in flats of mud or sand ("meadows") with depths of less than ten meters. These habitats must be sheltered from intense surf and oceanic swell, and often the best habitats occur behind offshore coral reefs and atolls, or in lagoons with small tidal effects and very clear water. In places where rock outcrops occur, seagrasses typically are replaced by algal macrophytes (seaweeds), although a few seagrass species occur in the surfweed community, attached to rocks below the level of lowest tide. Eelgrasses, Zostera marina and Z. pacifica, are species that occur in intertidal estuarine mud flats, but have also been located at a depth of 30 meters off the California coast; Zostera occurs as well in New England and northern Europe bordering cordgrass saltwater marsh (Spartina). Around Caribbean islands, turtlegrass (Thalassia testudinum) commonly occurs on the outer edge of Rhizophora, red mangrove. The remarkable record for depth is held by Halophila, found once at 90 meters in exceedingly clear water.

Taxonomy of Seagrasses

There are 12 genera of seagrasses, belonging to four monocotyledonous families.

  1. Family Cymodocaceae (17 species)
  2. Family Hydrocharitaceae (15 species)
  3. Family Posidoniaceae (9 species)
  4. Family Zosteraceae (16 species)

In external design, the halophytic seagrasses from different families can appear very similar, but evolution of these groups of genera has taken place several different times, quite likely early in the differentiation of monocotyledons, and likely from ancestors that inhabited brackish water of coastal salt marsh and estuary.

Some authors also list Ruppia maritima (Family Ruppiaceae) as a seagrass, whereas this species is generally not found beyond the margin of salt marsh.

Marine phanerogams have been observed along all continents except Antarctica (even though ironically one species is named Amphibolis antarctica!). Thirty of the 58 species are found around Australia, where much of the experimental work on seagrasses has been done. The largest seagrass meadow in the world occurs in the hypersaline Shark Bay of western Australia, where 12 species occur, but 85% of that coverage is by A. antarctica, which forms expansive monospecific stands. Shark Bay has very few rocky substrates, and the entire inlet is dominated by seagrasses. There are as many as 17 species in the general region of Perth, Australia in nearshore environments.

The rich assemblage of seagrasses around the continent of Australia produces a great amount of variation between localities. This differs greatly from the Neotropics, where there are only four major species, Halophila decipiens, Halodule wrightii, Thalassia testudinum, and Syringodium filiforme. Remarkably, there is only one tiny population of a seagrass, Heterozostera tasmanica, on the entire western coastline of South America, at Coquimbo, Chile. Absence of seagrass is attributed in large part to the lack of a protected, shallow, flat site with clear water.

General Features of Seagrasses

Because seagrass communities are highly productive, exceeding that of most crop plants, plant biologists have attempted to study in detail how carbon dioxide is delivered to the leaf chloroplasts across the waxy cuticle. Investigators know that at a typical ocean water pH of 8.2, as much as 99% of the carbon dioxide is present instead in the form of bicarbonate, HCO3. Speculation has been that bicarbonate, because it is so abundant, could be the carbon-containing molecule used. The best models to date, however, have revealed that carbon dioxide, a much smaller molecule, diffuses much more rapidly across the unstirred layer next to the leaf and through cutinized cell walls than does bicarbonate, so carbon dioxide is now taken to be the chief gas used to enter the leaf, even if present at a very low concentration.

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