CHAPTER VII

FLOATING CRUSTACEA OF THE OPEN SEA

It is only rarely that the floating organisms of the surface of the sea

are so large or so abundant as to catch the attention of the casual

observer. Except for an occasional shoal of porpoises or of flying-fish,

the waste of waters seen from the deck of a ship in mid-ocean usually

seems to be barren of life. Nevertheless, there is probably no region of

the ocean where the tow-net will not reveal the existence of a more or

less varied fauna and flora. Sometimes, indeed, these organisms, though

minute, are so numerous as to discolour the water over large areas;

whalers in the Arctic seas know by the appearance of "whale-food" where

whales are likely to be found, and Herring or Mackerel fishermen

recognize the changes in colour of the water among the "signs" which

guide them when and where to shoot their nets.

The organisms which make up this "pelagic" fauna and flora may be

grouped into two classes, which may be termed the "swimmers," or

Necton, and the "drifters," or Plankton. The former include the larger

and more active animals, such as fish, whales, and the like, whose

movements are more or less independent of the movements of the water;

the latter comprise the plant-life and the floating or feebly swimming

animals that drift at the mercy of waves and currents. A great deal of

attention has been given in recent years to the study of the plankton,

and it has come to be recognized as filling a very important place in

the balance of life in the sea. In the sea, as on land, all the animals

are ultimately dependent on plants for their food. The larger and more

conspicuous sea-weeds which grow on the sea-bottom, however, can only

flourish in comparatively shallow water, and the region which they

occupy forms only a narrow fringe round the land-masses of the globe. It

is only necessary to look at a map of the world, showing the depth of

the sea, to realize what an insignificant part of the area of the oceans

contributes in this way to the food-supply of marine animals. The

microscopic plant-life of the plankton, however, makes up for the

individual minuteness of its constituents by their incalculable numbers.

The lowly organisms known as "diatoms," familiar to the microscopist

from the beauty of their flinty skeletons, are among the most numerous

and important of these, and they are associated with a great variety of

other single-celled algae and allied organisms, some of them so minute

that they pass through the finest silk plankton-nets, and have to be

sought for by special methods of collection recently devised for the

purpose. All these organisms possess the green colouring matter

(chlorophyll) that enables them to live, as the higher plants do, on the

carbon dioxide and other substances dissolved in the water. The smaller

animals of the plankton feed on these vegetable organisms, and in their

turn serve as food for larger animals. The Herring, the Mackerel, the

gigantic Basking Shark, and the still more gigantic Greenland Whale, all

feed directly on the animal plankton, and we have already seen that the

animals of the deep sea depend entirely on the same source of

food-supply. Further, very many of the bottom-living animals of shallow

water swim at the surface in the early stages of their life, and feed on

the other plankton animals and plants. Indeed, it is no exaggeration to

say that "all fish is diatom" in the same physiological sense as "all

flesh is grass," and the study of the plankton is thus of practical

importance as well as of scientific interest.

Of all the minute animals that form the intermediate links in the chain

between diatom and fish or whale, the Crustacea are the most important

and the most numerous both in species and in individuals. The Copepoda

are more richly represented than any of the other groups, and it would

be difficult to find a sample of marine plankton from which they were

altogether absent. Associated with them we find one or two species of

Cladocera, a larger number of Ostracoda (chiefly of the family

Halocypridae), a few Mysidacea, the Amphipoda of the suborder Hyperiidea,

the Euphausiacea, and some of the shrimp-like Decapods; while the larval

stages of these and other groups also form an important part of the

plankton.

It is necessary to make a distinction between the "neritic" plankton of

shallow water near the coast and the "oceanic" plankton of the open sea.

In the inshore waters the plankton consists not only of organisms that

pass the whole of their life at or near the surface, but also, and very

largely, of the free-swimming larvae of bottom-living species, and of

others that make occasional and temporary excursions to the surface. For

example, if the tow-net be used a short distance from land--say in some

sheltered bay on our own coasts--the catch will often be found to

consist largely of larval Crustacea. The zoea and megalopa stages of

Crabs, the zoea and schizopod stages of Prawns and Shrimps, are often

conspicuous by their numbers, or we may find swarms of the nauplius and

cypris larvae of Barnacles. Sometimes, and especially at night, numbers

of Cumacea may be found in the tow-net; and it is noteworthy that these

are usually males, which leave the females burrowing in the mud at the

bottom, and swarm to the surface for a brief period of activity.

Besides all these more or less temporary visitors, however, there are

numerous species, even in the inshore waters, which are adapted to a

floating life, and pass their whole existence as members of the

plankton. Copepoda of many kinds, some Mysidae, Amphipods like

_Hyperia_--which is commonly found sheltering under large

jellyfish--some species of actively swimming Isopods, and many other

forms, are only to be captured by the tow-net; and now and then, in

certain localities, winds and currents may drive into coastal waters

shoals of species whose proper home is the open ocean.

In a similar way the strictly neritic forms may sometimes be carried far

out to sea, so that it is nowhere possible to draw a hard-and-fast line

between the regions occupied by the neritic and the oceanic plankton.

With increasing distance from land, however, the larval stages of

bottom-living species become fewer, and finally disappear altogether,

and there is left an assemblage of animals whose whole existence is

passed floating at the surface or at the intermediate depths. How far

down from the surface this floating fauna actually descends is a

question which has been much debated. It appears now to be certain that

there is no stratum of water between the surface and the bottom of the

ocean which is devoid of life, although the upper layers (not at, but

some distance below, the surface) are probably much more densely

populated than those of the abyss. Many of the species appear to

undertake more or less extensive migrations in a vertical direction,

coming nearer the surface at certain stages of their life-history, and

sinking into deeper water at others. Further, some species at least seem

to rise to the surface at night, and to sink again during the day. Apart

from these vertical movements, which are as yet only imperfectly

understood, it is desirable to distinguish between the "epiplankton,"

comprising the organisms which inhabit the superficial strata of the

ocean down to about 100 fathoms, and the "mesoplankton," found at

greater depths. The plant-life which is dependent on sunlight belongs to

the epiplankton, while the animals of the mesoplankton are dependent,

like the bottom animals of the deep sea, on the supply of dead food

material falling from above. A third division, the "hypoplankton," has

been established for those animals which live immediately above the

bottom, but its distinctness from the mesoplankton has not yet been

satisfactorily established. Indeed, many of the swimming forms which

have already been mentioned in dealing with the Crustacea of the deep

sea are probably rather to be considered as belonging to the deep

mesoplankton--at least, where their size and swimming powers do not

entitle them to be ranked with the "necton."

[Illustration: FIG. 48--_Conchoecia curta_, AN OSTRACOD OF THE PLANKTON.

x 40. (Partly after G. W. Mueller.)]

Many of the modifications in structure characteristic of pelagic

animals may be traced to the necessity for keeping continuously afloat

with a minimum of exertion. The Crustacea of the plankton never carry

the heavy armour found in bottom-living species. Thus, the thick-shelled

Ostracoda of the bottom are represented in the plankton chiefly by the

family Halocypridae (Fig. 48), in which the shell is thin, uncalcified,

and almost membranous. Many species, particularly of the Copepoda, are

seen, under the microscope, to have large globules of oil distributed

through the tissues of the body, and these no doubt serve as floats,

increasing the buoyancy of the animal. The same purpose is probably

served, in many cases, by having large spaces, filled with fluid, within

the body. This is characteristic of pelagic animals, and is well seen in

many of the Crustacea in which the viscera and muscles occupy a

relatively small part of the interior of the animals, the intervening

spaces being filled with colourless transparent fluid. Many of the

Hyperid Amphipoda show this peculiarity--for example, the relatively

gigantic _Cystisoma_, which is mesoplanktonic in deep water; and it

reaches its extreme in _Mimonectes_ (Fig. 49), in which the anterior

part of the body is, as it were, blown out into a balloon, giving the

animal the aspect of a small jellyfish rather than an Amphipod.

[Illustration: FIG. 49--_Mimonectes loveni._ A FEMALE SPECIMEN SEEN FROM

THE SIDE AND FROM BELOW, SHOWING THE DISTENDED-BALLOON-LIKE FORM OF THE

ANTERIOR PART OF THE BODY. x 3. (After Bovallius.)]

If, as seems probable, the body-fluid of these animals is of a lower

specific gravity than the sea-water, it will act like the oil-globules

of the Copepoda in keeping the animals afloat. Even if the specific

gravity be the same, however, the distension of the body with fluid

acts in another way, by increasing the surface exposed to friction with

the surrounding water, and so retarding sinking. The principle involved

is illustrated by the fact that a soap-bubble sinks much more slowly

through the air than the drop of water into which it collapses. The

same result is produced if the surface is increased by outstanding

spines or hairs, just as, for instance, a downy feather sinks slowly

through the air, but drops rapidly if it is rolled into a ball between

the fingers. This is, no doubt, one function of the spines with which

plankton Crustacea, and particularly larvae, are frequently provided,

though they may also serve in some cases as a protection against

enemies. The spines have been already alluded to in describing the

various larvae, but it may be noted here that they are most strongly

developed in larvae which live in the open ocean; for example, the most

elaborately armed of all Decapod larvae are the zoea stages of

_Sergestes_ (Fig. 50), which, like the adults, belong to the oceanic

plankton. The nauplius larvae of Cirripedes are all more or less spiny,

and the spines reach an exaggerated development in the larvae of the

genus _Lepas_ (Fig. 51), of which the adults are attached to floating

drift-wood or the like, and belong to the oceanic fauna, although hardly

to be classed with the plankton.

[Illustration: FIG. 50--THE ZOEA LARVA OF A SPECIES OF _Sergestes_,

TAKEN BY THE "CHALLENGER" EXPEDITION. x 25. (After Spence Bate.)]

[Illustration: FIG. 51--THE NAUPLIUS LARVA OF A SPECIES OF BARNACLE OF

THE FAMILY LEPADIDAE, SHOWING GREATLY-DEVELOPED SPINES. FROM A SPECIMEN

TAKEN IN THE ATLANTIC OCEAN, NEAR MADEIRA. x 11. (After Chun.)]

The large feathered bristles that decorate the limbs or tail of many

plankton Copepoda have no doubt the same function in assisting

flotation. In the genus _Calocalanus_ (Fig. 52), for example, the tail

setae are large and brilliantly coloured feathery plumes, and in one

species, _C. plumulosus_, one of these setae is of relatively enormous

size, five or six times as long as the body of the animal itself.

[Illustration: FIG. 52--_Calocalanus pavo_, ONE OF THE FREE-SWIMMING

COPEPODA OF THE PLANKTON. ENLARGED. (From Lankester's "Treatise on

Zoology," after Giesbrecht.)]

Among the most singular of plankton Crustacea are the _Phyllosoma_ larvae

(see Fig. 28, p. 72) of the Spiny Lobsters and their allies

(Scyllaridea), which have been already described. These larvae are

sometimes found far out at sea, and it seems likely that their larval

life is unusually prolonged, and that they may be drifted to great

distances by ocean currents. At all events, they are well adapted for

pelagic life, since the broad flat body, hardly thicker than a sheet of

paper, can be sustained in the water like a "hydroplane" by

comparatively slight efforts of the swimming legs.

The watery character of the body, together with the thinness of the

exoskeleton, helps to explain the glassy transparency which is a feature

of most plankton Crustacea. This transparency has been regarded as a

protective adaptation rendering the animals inconspicuous in the water,

and it has indeed that effect to human eyes, but it is very doubtful

whether the animals derive much benefit from this. Many of the

animals--such as Herring and other pelagic fishes--that prey upon

plankton Crustacea appear to swallow them in bulk, without much

selection; and the Greenland Whale, as it swims open-mouthed through the

sea, is not likely to be guided by the greater or less visibility of the

Copepods that it sifts out on its baleen plates. Further, this

glass-like transparency is by no means universal, for many plankton

Copepoda are brightly coloured. In some, as in the beautiful blue

_Anomalocera_, common in British waters, the colour is due to pigment in

the fluids and tissues of the body; in others the feathery hairs on the

body and limbs show brilliant metallic colours, produced, like the

colours of a peacock's feather, not by pigments, but by the diffraction

of light in the texture of the organ. The most beautiful of all Copepoda

is _Sapphirina_, in which the surface of the body absolutely sparkles

with iridescent colours.

The striking phenomenon known as the "phosphorescence of the sea" is

familiar to every ocean voyager, and is seen from time to time on our

own coast. On a dark night the crest of every wave often seems to break

in a pale glow, the wake of the vessel is a trail of light, and an oar

dipped in the water seems on fire. This luminosity is due to the animals

of the plankton, largely to the lowly Protozoa and the jellyfishes, but

in part also to certain Crustacea. A number of pelagic Copepoda have

been shown by Giesbrecht to secrete, from special glands on the surface

of the body, a substance which becomes luminous on coming in contact

with the water. Even specimens which had been dried were found to give

out light on being wetted. Some pelagic Ostracods of the family

Halocypridae have been observed to emit clouds of a luminous secretion

from a gland in the neighbourhood of the mouth. A similar habit has been

seen, as already mentioned, in certain deep-sea Prawns and Mysidacea,

which may perhaps belong to the deeper part of the mesoplankton rather

than to the bottom fauna. The complex light-producing organs of the

Euphausiacea have already been described in dealing with deep-sea

Crustacea. A great many species of this group, however, are members of

the epiplankton, and in these the phosphorescent apparatus is quite as

fully developed as in species coming from greater depths.

_Meganyctiphanes norvegica_ (Fig. 24, p. 56), which is one of the

largest of the Euphausiacea, is common at no great depths in many places

in British seas. If a jar of sea-water in which specimens of this

species are swimming be brought into a dark room, a tap on the glass

will cause the photophores to flash out like a row of tiny lamps along

the side of the body. After shining for a few seconds the light dies

out, to appear again if the tapping be repeated.

There are certain peculiarities in the structure of the eyes in some

plankton Crustacea which suggest that the sense of sight is of special

importance to their possessors, although we can hardly do more than

guess at their special significance. Most Copepoda have only a single

eye in the middle of the head, corresponding to the single eye of the

nauplius larva, and of far simpler structure than the paired compound

eyes of most other Crustacea. In many plankton species, however, this

simple eye becomes much enlarged and complicated in various ways. The

three parts of which it is normally made up may become separated from

each other, and are sometimes increased in number to five, while lenses

serving to concentrate the light are often developed by thickening of

the overlying cuticle. The most elaborately constructed eyes are found

in the family Corycaeidae. In _Copilia_ (Fig. 53) a pair of eyes of

relatively enormous size are present. Each has in front a large biconvex

lens set at the end of a conical tube which extends backwards to a

smaller lens (like a telescope with object-glass and eyepiece), behind

which, again, are the sensory cells, corresponding to the retina,

enclosed in a tube of dark pigment, the whole apparatus being more than

half the length of the body. These eyes, although paired, do not

correspond to the paired compound eyes of other Crustacea, but have

arisen by the separation and enlargement of two of the three divisions

of the typical median Copepod eye.

[Illustration: FIG. 53--_Copilia quadrata_ (FEMALE), A COPEPOD OF THE

FAMILY CORYCAEIDAE, SHOWING THE PAIR OF LARGE "TELESCOPIC" EYES. x 20.

(After Giesbrecht.)]

A peculiarity of the paired compound eyes found in plankton Crustacea of

several different orders consists in the division of each eye into two

parts, which differ in structure. In many Euphausiacea and Mysidacea,

especially in those haunting the deeper strata (mesoplankton), this

division of the eyes is well marked, a frontal or dorsal part having the

separate elements of the eye (ommatidia) greatly lengthened and with

reduced pigment, while the lateral part is of more normal structure. It

seems probable, from the researches of Professor Chun, that the

fronto-dorsal division is adapted for the perception of very faint

light, while the lateral division will give a more accurate image of

brightly illuminated objects.

[Illustration: FIG. 54--_Phronima colletti_, MALE. FROM A SPECIMEN TAKEN

IN DEEP WATER NEAR THE CANARY ISLANDS. x 12. (After Chun.)]

In the pelagic Amphipoda, forming the suborder Hyperiidea, the eyes are

of very large size, generally occupying almost the whole surface of the

head, and giving the animals a very characteristic appearance, in

contrast to the small-eyed, bottom-living Gammaridea. In the family

Phronimidae (Fig. 54) the eyes are each divided into two parts, differing

in structure in the way just described.

There are a few Crustacea living habitually on the high seas which

cannot be reckoned as belonging either to the true plankton or to the

necton, since they depend on outside help for keeping themselves afloat.

Among these are the Barnacles which cluster on logs of drift-wood, and

are among the most important causes of the "fouling" of ships' hulls on

long voyages. The stalked Barnacles of the genus _Lepas_ are especially

common in such situations, and the characters of their larvae have been

already alluded to. Certain species of sessile Barnacles are constantly

found attached to large marine animals. For example, _Chelonobia_

adheres to the shell of Turtles, while _Coronula_ and some allied genera

are found on Whales.

[Illustration: _PLATE XIX_

_Latreillia elegans_, ONE OF THE DROMIACEA WHICH RESEMBLES A

SPIDER-CRAB. FROM THE MEDITERRANEAN. (NATURAL SIZE)

THE GULF-WEED CRAB, _Planes minutus_. (SLIGHTLY ENLARGED)]

The little "Gulf-weed Crab" (_Planes minutus_--Plate XIX.) is found

clinging to floating drift-weed nearly everywhere throughout the

temperate and tropical seas of the globe, and is especially common in

the area known as the Sargasso Sea, in mid-Atlantic. It is occasionally

drifted to the south coasts of the British Islands. In Sloane's "Natural

History of Jamaica," published in 1707-1725, it is stated of the

Gulf-weed Crab that "Columbus, finding this alive on the Sargasso

floating in the sea, conceived himself not far from some land, on the

first voyage he made on the discovery of the West Indies."

A few other Crustacea also form part of the peculiar fauna which is

associated with the Sargasso weed, notably a swimming Crab, _Neptunus

sayi_, and two or three species of Prawns. All of these are coloured

olive-green, like the weed among which they live.

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