SMS 322 Biology of Marine Vertebrates Spring 2001 Diversity of Habitats in the Oceans Occupied by Vertebrates January 30 Reading assignment: Helfman et al. Pages 295-309 of Chapter 17; Lutz and Musick Chapter 6; Berta and Sumich Chapters 2-5 (as suggested by Ione). 1. 2. Following brief introduction to who the marine vertebrates are, let’s look at where they live in a general sense. There are a at least three instructive ways to slice the oceans to examine zones or habitats occupied by marine vertebrates. a. The first is a general classification used by oceanographers and marine biologists, which separates into zones the water and the bottom portions of the oceans, based partly on depth and partly on physical features of the oceans. Marine vertebrates occur in all the zones I’m about to define. (See Fig. 9-1 from Pinet (2000).) i. ii. iii. The pelagic province (or zone or realm) is the ocean water from the bottom to the surface, i.e., what oceanographers call the water column. The benthic province is the sea bottom. The pelagic province is divided horizontally into the neritic and oceanic zones. (1) (2) i. Neritic zone is the water column over the continental shelves, defined loosely as the zone from the shore to the continental shelf break, where the slope of the bottom increases sharply (usually at about 150-200 m depth). Zone may be 1000 km wide as in parts of the Arctic ocean or only a few km wide as along the west coasts of N. and S. America. Oceanic zone is the water column beyond the shelf break. The oceanic zone is divided vertically into five pelagic zones. (1) (2) Epipelagic zone, arbitrarily from 0-200 m, but it roughly corresponds to the depth of the shelf break and the depth of significant photosynthesis in the clearest ocean waters. Important because here is where almost all primary productivity occurs, driving food production for marine vertebrates. Mesopelagic zone, arbitrarily from 200-1000 m, with the faintest downwelling sunlight becoming undetectable in the (3) (4) (5) i. The benthic province is also zoned vertically by depth. (1) (2) (3) (4) (5) (6) i. a. zone. Food for marine vertebrates or their prey below the epipelagic zone must be carried down by critters or rain down by gravity. Bathypelagic zone, arbitrarily from 1000-2000 m. Abyssalpelagic zone, arbitrarily from 2000-6000 m. Hadalpelagic zone, from 6000 m to bottom, basically the deep-sea trenches so this definition isn’t quite so arbitrary. (Hades=god of the netherworld and dispenser of earthly riches in Greek mythology; underground abode of the dead; hell.) Supralittoral zone is above high tide line but influenced by salt spray; not of major concern to us except that many marine vertebrates use this zone for reproduction, basking, or sometimes feeding. Littoral zone is the extent of sea bottom between high and low tide lines. Sublittoral zone is the sea bottom from low tide line to the continental shelf break, again usually 150-200 m deep. Bathyal zone is sea bottom from 200-2000 m. Abyssal zone is sea bottom from 2000-6000 m. Hadal zone is sea bottom below 6000 m. The abyssalpelagic zone and the abyssal benthic zones have by far the greatest volume and area, while the epipelagic zone and sublittoral benthic zone, where primary production occurs, have small volume and area. (See Table 9-1 from Pinet (2000).) We might slice the oceans from pole to pole; I just do this briefly to illustrate some extremes. Vertebrates occur in all areas of the hypothetical slice. i. ii. iii. iv. Arctic Ocean, ice-covered water year-round in the polar region; no continent; coldest water in the world’s oceans at the bottom of the Arctic (below 0 C). Temperate oceans north and south, usually ice-free except bergs or near-shore winter ice; cold water deep all year; summer surface temperatures to about 20 C. Sub-tropical and tropical oceans; cold water deep all year; surface temperatures greater than about 18 C all year; surface temperatures in tropics >25 C to as much as 32 C in western Pacific. Antarctic or Southern Ocean surrounds continent of Antarctica; fringed with ice of seasonally greater or lesser extent; also sea v. temperatures below 0 C. The zones along this north-south slice are defined by oceanographic features. (1) (2) (3) (4) (5) a. Thirdly, we might look at specific habitat types, sometimes defined by a bottom type, but perhaps including the overlying water column. No detail now, but some examples. i. ii. iii. iv. v. vi. 1. Polar seas occur poleward of oceanographic features called polar convergences. Temperate seas occur between polar convergences and subtropical convergences. Subtropical seas occur equatorward of subtropical convergences. Tropical seas occur surrounding equatorial current regions. The separations between polar, temperate, and subtropical areas are where surface temperatures change rapidly and frequently demarcate faunal changes, at least in the epipelagic zone. In shallow tropical seas, mangroves, coral reefs, and sandy bottoms. From the littoral to the abyss, mud substrates. In polar seas, the ice edge. In the Gulf of Maine, rocky intertidal and subtidal areas. The air over the oceans doesn’t fit neatly into any of our classifications, but is clearly important for sea birds. Adjacent land doesn’t fit neatly either, but is clearly important for some marine reptiles, birds, and mammals. Now let’s look at who lives where and why in a general sense. a. b. c. I’ve given you a lot of terms, but as I talk about where marine vertebrates are, remember our goal of developing a perspective. We might consider what some of the constraining factors are in considering where marine vertebrates dwell. We’ll consider zoogeography specifically later, but now let’s see what types of marine vertebrates live in some of the areas mentioned in our classification “slices.” Consider this Gary Larson cartoon. Gary is a zoologist turned cartoonist, but what is wrong with this picture? i. ii. Polar bears and penguins both adapted to polar conditions and inhabit the edge of the ice, but they wouldn’t be found on the same cake of ice. Polar bears are endemic to the Arctic and all penguins are endemic iii. to the southern hemisphere, with several endemic to the Antarctic. Vertebrate faunas of the Arctic and Antarctic oceans are quite distinct, with more endemic species in the Antarctic than in the Arctic. I said zoogeography later, but just to finish the thought: (1) (2) (3) Antarctic Ocean has had cold climatic conditions, and has been well separated physically and oceanographically from other areas, for about 25 million years–lots of time to evolve endemic species. Arctic Ocean is more directly connected to north temperate seas, and it has had repeated warming and cooling until cold conditions stabilized only about 3 million years ago–not so much time for endemism to develop. This is not to suggest there is no overlap in Arctic and Antarctic vertebrate faunas. (a) (b) a. Fishes are found everywhere in the marine environment; reptiles, birds, and mammals are not. Why not? What is a major constraining factor in habitat diversity of the latter groups? i. ii. a. Arctic terns, e.g., nest along the northern rims of the northern hemisphere continents, i.e., at the edge of the Arctic Ocean and on its islands. In autumn, they migrate to the Antarctic where they feed during austral summer at the edge of the ice pack. They gotta breathe air. Thus, even though some may dive into the mesopelagic or sometimes bathypelagic zones, all the reptiles, birds, and mammals are epipelagic (or aerial) most of the time. Let’s start with the mammals and work down to the fishes. Where are the marine mammals with respect to our slices? A major habitat dichotomy is based on another constraint, the necessity in some to give birth or perform other necessary functions on land. i. Those tied to land at least at some stage in life cycle. (1) (2) Sea otter (Order Carnivora, Family Mustelidae) is neritic, seldom going more than 2 km offshore, and temperate to subarctic along North Pacific coast of North America. Quite marine despite coastal distribution. Usually stays at sea except in storms, but some sleep ashore. Give birth on shore, but soon return to sea with pup. Polar bear (Order Carnivora, Family Ursidae) is really land or (3) ice based, entering the sea to feed (even on small belugas). However, most of its hunting is of marine mammals on the ice (various seals, walrus). It is north polar as noted. Tied to marine food chain for sure–call it a marine mammal or not. “Pinnipeds” (Order Carnivora, sometimes Suborder Pinnipedia) are in three families. They all haul out on ice or land to rest, sleep, vie for mates, breed, or give birth. (a) (b) (c) (d) (e) i. The walrus (Family Odobenidae) is Arctic in distribution, and is neritic, feeding on benthic invertebrates, esp. molluscs. The eared seals (Family Otariidae) (8? fur seals and 5 sea lions). The true seals (Family Phocidae) (??) haul out, but they are clumsier on land or ice than the other pinnipeds. These are either neritic or associated with pack ice over deep water; though they all haul out, some are deep divers into the mid-mesopelagic zone, as we will discuss later. Most are polar or temperate, but a few species are found in tropical regions, e.g. in the eastern Pacific Ocean. Those not tied to land. (1) (2) Manatees and the dugong (Order Sirenia) are coastal or estuarine (or freshwater) in tropical and subtropical waters. Because they eat attached aquatic vegetation, they are restricted to shallow near-shore waters, though they never come onto land. (Steller’s sea cow was an Arctic sirenian that humans extinguished in just a quarter-century after its discovery by European explorers.) The remaining mammals (Order Cetacea, the whales, dolphins, porpoises) are still less tied to land or the ocean margins. However, there is still considerable variability in where in the ocean slices particular species are found. Some are highly migratory as well. (a) (b) (c) Gray whales (Family Eschrictiidae), e.g., are highly migratory but quite coastal in distribution along Pacific coast of N.A. Beaked whales (Family Ziphiidae) are poorly known, in part, because they are oceanic pelagic over the deep oceans away from land. Sliced another way, there are Arctic species (narwhal and beluga) all the way to Antarctic species (pygmy right whale). a. Where are marine birds with respect to our habitat slices? Let’s let our perspective again be on constraints to habitats occupied by sea birds. Arguably, there are 20 or so families that contain sea birds or birds dependent on the sea. All must lay eggs on land, so in contrast to marine mammals, all are tied to the land at some stage. i. ii. There is probably not a dichotomy, as in marine mammals, but rather a continuum of use of the marine environment by different groups or species of birds. Here’s an example contrast. Two groups of tropical and subtropical birds that spend lots of time flying or soaring over the ocean feeding primarily on fish are the tropicbirds (Family Phaethodontidae) and the frigatebirds (Family Fregatidae). (1) (2) i. ii. a. Frigatebirds cannot walk or swim. They fly above the ocean and swoop down to catch fish at surface or steal food from other birds. They return to land at night to roost in trees. They are primarily above the neritic zone. Tropicbirds fly above and then plunge into water to catch food. Outside the breeding season they are truly pelagic, remaining far from land for long periods. Cormorants (Family Phalacrocoracidae) range as different species from Arctic through temperate, tropical, regions to Antarctica. All are neritic, needing to dry their wings periodically, as the feathers are not completely waterproof. Albatrosses (Family Diomeidae) range as different species from Antarctica to north temperate (in Pacific), but the juveniles and non-breeding adults wander far from land for long periods. How about the marine reptiles? All tied to land by need to lay eggs. i. ii. Marine iguana spends lots of time on land venturing into water near shore to feed. Definitely neritic. At the other extreme are some of the sea turtles. (1) (2) (3) Early juvenile loggerheads, green turtles, and probably leatherbacks and hawksbills are found all over the North Atlantic, e.g., and may be in the open sea for one to several years. Definitely oceanic pelagic. (Some are in other oceans too.) Early juvenile Kemp’s Ridleys are all over the Gulf of Mexico. Flatbacks on the other hand seem to be neritic from the (4) i. a. b. start. After greater or lesser time, they recruit back to neritic regions, bays and estuaries and take up a more benthic oriented style. Slicing north to south, the marine reptiles are tropical, subtropical, and maybe a bit temperate. (Why no polar marine reptiles? Food for thought–ectothermy and air breathing may not be compatible for moderate to large animals.) Before going to the fishes, there is another major constraint on distribution of marine vertebrates with respect to zones or habitats (although the constraint applies to fishes, too). There are numerous species and numerous populations around Antarctica–lotsa birds, lotsa whales, lotsa seals. Ditto for the west coasts of North and South America. Contrast with the Sargasso Sea in the middle of the North Atlantic gyre, where one seldom sees a whale or bird or turtle. Most of the air breathing marine vertebrates are predators, often top predators, and they are diverse and abundant where oceanic productivity is greatest. Now, the 15,000+ marine fishes. Fishes occupy the greatest diversity of habitats by far among the marine vertebrates. i. Air-breathing (therefore epipelagic) constraint removed, so fishes can be and are distributed from the surface to the deep sea, though a given species can’t be. ii. Pressure, light, temperature, sheer volume, and food are increasing constraints from the surface downward. Discuss these in detail later, but a few key points for the oceanic (not neritic) groups. (1) (2) Pelagic species are generally countershaded, usually streamlined, good swimmers, with well developed but not extreme eyes, often schooling and often migratory. They have efficient respiration and food conversion capability. Most of the bony fishes in this zone have swim bladders (gas bladders) for buoyancy control. Mesopelagic species generally have large swim bladders, enlarged specialized eyes, specific patterns of bioluminescence. Most are relatively small, and they have good ability to regulate swim bladder volume. Many make diurnal vertical migrations into the epipelagic at night. (a) (b) Temperature decreases with depth, rapidly at any thermocline, and is always cold in the lower mesopelagic and deeper zones. DVM species may cope with considerable temperature change daily–unusual among oceanic marine fishes. (c) (1) i. Examples from 22 families of eels. We can slice from the shore out, too. (1) (2) (3) (4) i. Fishes in the deeper zones tend to have reduced or vestigial eyes, reduced skeletons, reduced musculature, and reduced metabolism. They have no swim bladders or swim bladders filled with lipid instead of gas. Many have very large mouths. Adaptations to a low sporadic food, high pressure environment. So we’ve got this tremendous range of vertical distribution of species, but damn near every oceanic species has epipelagic larvae. This means that larvae may develop under conditions much different than those under which the juveniles and adults dwell. The reasons I’ll leave for Ione for later. However, one often reads about vertical distributions and characteristics of fishes, but those almost always refer to adults. (1) i. Some widespread mesopelagic species are deeper in tropical than temperate regions, socalled tropical submergence. A few species can breathe air, or can supplement with air. This opens the littoral zone to some even at low tide (mudskippers, blennies). In contrast to the other vertebrate groups, small body size of many fishes allows exploitation of interstitial habitats especially in neritic waters (coral reefs, tunnels, under rocks, etc.). Benthic habitats are more fully occupied in the neritic zone, e.g. by flatfishes, skates, sculpins, etc. Pelagic fishes in the neritic zone do or do not conform to the characteristics of the oceanic pelagics in coloration, body shape, etc. Sliced from pole to pole takes us from endemic Arctic species through the zones to a large number of endemic Antarctic species. Many mesopelagic and deeper species have very widespread distributions, because similar temperature conditions may be found over large areas of the oceans. (1) (2) The polar species cope with water temperatures below 0 C by having antifreeze glycoproteins which lower the freezing point of their tissues fluids. Antarctic species have numerous other interesting adaptations as well.