THE GEOGRAPHICAL DISTRIBUTION OF FISHES.

There are known at the present about twenty thousand species of fishes,

which are distributed throughout the creeks, rivers, lakes, seas and

oceans of the world. A few species of the open sea are cosmopolitan;

the others are more or less restricted in their range. Northern Asia,

Europe and North America have in common a few species of fresh water

fishes. There are many others of close relationship, which indicates a

somewhat common origin of the fish faunas. The same is largely true of

the salt water shore fishes, which live well to the north. The fresh

water fishes of South America, Africa and Australia are all different

from each other, none being even closely related as are those we find

in the countries of the northern hemisphere.

The fishes of our Atlantic coast are different from those of the

Pacific, very few species being common to both coasts. The fishes of

the Ohio river are entirely different from those of the Columbia, not a

single species being common to both streams. The fishes of the Missouri

river are very different from the Ohio, many of the larger species, as

catfishes, buffalo fishes, black basses, and some of the sun fishes are

common to both rivers. The difference between the fishes of these two

rivers is chiefly in the smaller kinds, which do not migrate to any

great extent, and is greater as you go toward their sources, or confine

yourself to their smaller tributaries.

There are many reasons why the fishes of one region are not the same as

those we find in another. Some of these reasons we may learn by making

a careful study of the fishes of each region, and their environment.

In addition we must learn all we can about the past history of the

country, finding which streams were formed first, and how they became

inhabited from the old ancient fish faunas of our earlier geological

periods. If you visit streams in the Alleghanies, the Ozarks and the

Black Hills you will find them much alike. All have clear, cool water,

flowing over sand or gravel. The black bass, speckled trout, channel

cat, and the eastern pickerel will live quite as well in streams of

each locality. If you spend a day at each place collecting fishes all

your catch will not be the same species. In the Alleghany region you

will obtain about forty species, and a like number in the Ozarks. Of

these quite one-fourth, or one-fifth, will be the same species, and

the others closely related. A large portion will consist of sunfishes

and very small, perch-like fishes, which are called darters. These are

spiny-rayed fishes; that is, nearly all of the fins are made partly of

strong, sharp spines, such as you find on the back of sunfishes, black

bass and the like. In the streams of the Black Hills you will not find

more than fifteen species, and not more than one or two, if any, will

be the same as in either of the other two catches. There are none of

the spiny-rayed fishes in the Black Hills, and no trout, though the

streams seem in every way well suited for them. The fishes of the Black

Hills consist of two catfishes, four suckers, eight minnows, and one

member of the cod family. Why are there no spiny-rayed fishes? If you

examine a map you will find that the Black Hills is an isolated region,

about seventy-five by one hundred miles in extent. It is covered with

heavy pine forests and drained by a dozen or more good-sized creeks,

which find, through the north and south forks of the Cheyenne, an

outlet into the Missouri river. Surrounding the Black Hills is a broad

plain one hundred or two hundred miles in width. It has no forests, and

only a scant vegetation. Its streams are alkali and contain much solid

matter in suspension. None of these streams flow over rocky or gravelly

beds. Like all the streams of the great plains they are overloaded

with sediment. All the streams can do with this sediment is to deposit

it in places during falling or low water, and in time of freshets,

pick it up, shift it about and redeposit it farther down the stream.

Such streams are like the Platte, narrow and deep in a few places,

but mostly wide and shallow, with a bottom of quicksand. The streams

of the plains have in them but few species of fishes; especially is

this true of the upper Missouri, and these are such species as we find

in the Black Hills. It is thus evident that the fishes of this region

migrated there, and only such fishes as were able or willing to live

in the muddy, alkaline streams of the great plains could have ever

reached the Black Hills. The minnows and suckers are ever preyed upon

by sunfishes, bass and the like, and to escape them evidently sought

retreat in the alkaline water, which was too much disliked by their

enemies for them to follow. Once there and accustomed to such water

they would migrate farther up stream until they reached the clear, cool

streams of the Black Hills. If we compare the fishes of two rivers

whose mouths are near each other, as the Ohio and the Missouri, those

fishes found near the mouths will be the same species and the two river

faunas will differ most as you go toward their sources. On the other

hand, if you select two rivers whose sources are near each other, as

the James and tributaries of the Ohio, then the fish faunas will differ

most as you go towards their mouths. The same is true of the Missouri

and the Columbia. In such cases it often happens that during high water

some fishes are able to pass from the head waters of one river basin to

the other, just as we see the trout from the Columbia at the present

time colonizing the upper Yellowstone through the Two Ocean Pass. Near

the head waters of many mountain streams there is usually a pass, which

contains a strip of meadow land where the small streams from mountains

unite, forming the sources of two great rivers flowing in opposite

directions. This is the case both at the Two Ocean Pass, the source

of the Missouri and the Columbia, and at the point where the Canadian

Pacific Railroad crosses the divide, forming the source of the Frazier

and Saskatchewan rivers.

Many mountain streams whose sources are at present in no way connected

may have been so at no very remote period. All of our streams which

have their sources within the glaciated area were no doubt connected

as the ice receded. The drainage of Lake Champlain and the lakes in

central New York was southward at the close of the glacial epoch. It

is said that in times of high water one may pass in a skiff from the

head waters of the Mississippi to the Red River of the North. With such

facts before us we can easily understand why the fishes of two rivers

whose sources are near each other should be most nearly alike nearest

the divide. If the two rivers were formed about the same time, as no

doubt were the James and the Ohio, they would naturally have several

species in common. In other words, the two fish faunas will resemble

each other throughout their whole extent. In the case of the Missouri

and the Columbia, the former is much the older stream, and while their

sources have fishes common to both streams, in the lower parts of the

rivers the fish faunas are entirely different. The upper Missouri river

and its tributaries are for the most part inhabited by Rocky Mountain

fishes, practically the same fauna as we find in the Columbia, but few

species characteristic of the Mississippi valley have been able to even

cross the great plains and none have ever passed the Rocky Mountain

divide.

In the study of the geographical distribution of our fresh water

fishes, we are able to make a few generalizations as follows: Two

rivers in the same latitude, and belonging to the same great drainage

basin, and draining similar areas, will have similar fish faunas.

Thus we find a great similarity in the fishes of the Washita and the

Tennessee rivers, a much greater similarity than we do in the fishes

of the Washita and the Cedar rivers. If the stream is a large one,

the fishes near its source will be much unlike those near its mouth.

The fishes of Minnesota differ greatly from those of Louisiana,

though the drainage of these two States is in the Mississippi river

basin. Limestone streams have in them more species of fishes than do

sandstone. All things being equal, the larger of two or more streams

will contain the most species of fishes. There are few, if any, rivers

as rich in species as the Mississippi river and its tributaries. It

drains one slope of each of our two great mountain systems, besides

an immense area of wood-land and prairie, and numerous swamps and

marshes. Its upper course and many of its upper tributaries lie in

the region once covered by glaciers, though now traversed by great

moraines. Its fishes are as diversified as the area it drains. In its

mountain streams we find such fishes as the trout, darters, minnows

and suckers. In the upland streams are darters, shiners, suckers,

sunfishes and small-mouthed black bass. In the channels of the larger

tributaries are found the large suckers, buffalo fishes, gar pike,

channel catfish, drum, pike and pickerel. The lowland streams contain

the dogfish, pirate perch, some sunfishes, the large-mouthed black

bass, some suckers, catfishes and other species. Minnows, darters,

suckers and sunfishes are found in lowland, upland and mountain

streams, though not the same species in each. These fishes belong to

families which are made up of many species, some being strictly upland,

others strictly lowland, each having a limited range. In the same way

we have fresh water fishes and salt water fishes; some fishes, as the

trout and salmon and eel, live in both salt and fresh water. Many

other fishes, as the killifishes, thrive best in brackish water. Each

species of fishes is best fitted for a particular region into which it

has been forced to live, either to escape its enemies or to be able to

get a living easiest. In its migrations it has moved along lines of

least resistance, and has colonized those streams where Mother Nature

has been able to do the most for it. The darters are small, perch-like

fishes, which seldom exceed a length of six inches, the average being

about three. All are active and swift swimmers and well suited for

a life among the rocks and swift water of our smaller streams. All

countries have small, swift, rocky streams, but few have darters. In

their stead we find loaches, gobies, characins, sculpins, and the like.

These fishes have "become dwarfed and concentrated, taking the place in

their respective habitats which the darters occupy in the waters of the

Mississippi valley. By the same process of 'analogous variation' the

cichlids of South America parallel the sunfishes of the United States,

although in structure and in origin the two groups are diverse."

Dr. Jordan tells us that the trout of the Pacific coast came to America

from Asia, and gradually spread eastward and southward until now it is

found in all the streams of the Rocky Mountains, the Sierra Nevada, the

Cascades and the Coast range. It is but a short distance from Kamchatka

to Alaska, and this distance is traveled by trout to this day; once

over, a fish able to spend much of its time in salt water could easily

colonize all our coast streams. Whether or not all of our Pacific trout

are descendants of one species, the cut-throat trout, is more or less

uncertain, though it is quite certain that all have descended from not

more than two or three species. In many places they have been able to

pass from the head waters of one river to that of another, just as they

now pass from the head waters of the Columbia to the Missouri by the

way of Two Ocean Pass. The ancient lakes, Lahontan and Bonneville, no

doubt assisted them in their migrations. Since these have disappeared

each colony has had to remain more or less isolated. In time they

have become somewhat changed, to better adapt themselves to their new

environment. These changes have developed certain peculiar characters,

by means of which we can distinguish one kind of trout from another,

just as the farmer distinguishes his Berkshire from his Poland China.

Spread, as the trout are, over such a large area, in such an immense

variety of streams and lakes, and with a vertical range of over one

thousand feet, we would certainly expect as large a number of species

and varieties of trout to be developed as we find at present in the

streams of our west coast.

Fishes are found in the deepest parts of the ocean. Some of these

are peculiar to the deep waters, none of the shore fishes resembling

them. On the other hand, many deep sea fishes belong to families well

represented in the shallow water. The flounders are found in water at

all depths, and the same is true of the bat fishes, rock fishes and

other shore fishes. It is easy to understand how these fishes have

found their way to the deep water. It was either to escape their

enemies or to extend their range for some reason; as Mr. Garman puts

it, "They have slid down," as it were to the bottom of the ocean.

In general, animals migrating will always move along lines of least

resistance. Some deep-sea fishes have a considerable vertical range. It

is thought that some move into shallower water to deposit their eggs or

place their young in warmer water, and where the peculiar kind of food

they need early in life is the most abundant. To study deep sea fishes

is difficult, and so little has been done that we not only know them

imperfectly but also know very little concerning their life histories.

In February, March and April of 1891 the United States Fish Commission

steamer Albatross explored a portion of the region between the

coasts of Mexico and Central America and the Galapagos Archipelago.

Besides obtaining a large number of shore fishes, about nine hundred

specimens of fishes were secured, ranging from a depth of one hundred

to twenty-two hundred and twenty-three fathoms. This collection was

carefully studied by Professor Garman, of Harvard. He found the

collection to contain one hundred and eighty species, eighty-five

per cent. of which were new to science. The bottoms of the oceans

are far from level, and each deep basin has its own peculiar fauna.

The shallower parts of the sea prevent migration of the deep water

forms and no doubt living as they do in eternal darkness and in a

temperature near the freezing point, there is little to induce them

to much activity. The fact that they are easily captured in nets of

comparatively small size would indicate that they move about slowly.

Dr. Jenkins, who has lately studied the fishes of the Sandwich Islands,

informs me that less than five per cent. are found on our American

coast, while a large per cent. is found all the way to the Red sea.

In other words, the fishes of the Sandwich Islands are East Indian

rather than American. This is no doubt caused from the fact that the

deep water between the islands of the American coast forms a barrier

which has always prevented the two fish faunas from mingling with each

other. Between Africa and the Sandwich Islands this has not been the

case. A recent study of the fishes of the Galapagos Archipelago shows

its fauna to be American, though in what respect its fishes differ from

those of our west coast they resemble all the more the fishes of the

Sandwich Islands. Two fish faunas will usually differ from each other

if separated by an impassable barrier; especially is this true if the

barrier be older than the two faunas.

Any barrier which prevents or hinders fishes in their movements from

one body of water to another will separate two more or less well-marked

fish faunas. These barriers may be mountains, or shallow water, as in

the case of deep sea fishes; deep water, as in case of shore fishes;

muddy or alkaline water, or water of different temperature. Temperature

no doubt has far more influence in governing the movement of fishes

than is generally believed. It plays an important part in guiding

salmon up stream to their spawning beds. It explains why they reach the

head waters of some streams and spawn earlier than in similar streams

not far distant, but of different temperature. If you would know to

what extent fishes of one region differ from those of another, study

well the barriers between the two regions, learn to what extent and

how long they have existed, consider the age geologically of the two

regions, and how fishes may have migrated to one or the other, and in

a general way you will have the key to the situation, which a careful

study of the fishes is quite sure to verify.

Seth E. Meek.

[Illustration: LOUISIANA TANAGER.

(Piranga ludoviciana.)

Life-size.

FROM COL. CHI. ACAD. SCIENCES.

COPYRIGHT 1900, BY

A. W. MUMFORD, CHICAGO.]

Birds and Nature, Vol. 08, No. 4, November 1900 Illustrated by Color Photography · 第 14 / 22 题