further check upon their migrations. In these respects almost all other
organisms have great advantages over mammals. Birds can often fly long
distances, and can thus cross arms of the sea, deserts, or mountain
ranges; insects not only fly, but are frequently carried great distances
by gales of wind, as shown by the numerous cases of their visits to
ships hundreds of miles from land. Reptiles, though slow of movement,
have advantages in their greater capacity for enduring hunger or thirst,
their power of resisting cold or drought in a state of torpidity, and
they have also some facilities for migration across the sea by means of
their eggs, which may be conveyed in crevices of timber or among masses
of floating vegetable matter. And when we come to the vegetable kingdom,
the means of transport are at their maximum, numbers of seeds having
special adaptations for being carried by mammalia or birds, and for
floating in the water, or through the air, while many are so small and
so light that there is practically no limit to the distances they may be
carried by gales and hurricanes.
We may, therefore, feel quite certain that the means of distribution
that have enabled the larger mammalia to reach the most remote regions
from a common starting-point, will be at least as efficacious, and
usually far more efficacious, with all other land animals and plants;
and if in every case the existing distribution of this class can be
explained on the theory of oceanic and continental permanence, with the
limited changes of sea and land already referred to, no valid objections
can be taken against this theory founded on anomalies of distribution in
other orders. Yet nothing is more common than for students of this or
that group to assort that the theory of oceanic permanence is quite
inconsistent with the distribution of its various species and genera.
Because a few Indian genera and closely allied species of birds are
found in Madagascar, a land termed "Lemuria" has been supposed to have
united the two countries during a comparatively recent geological epoch;
while the similarity of fossil plants and reptiles, from the Permian and
Miocene formations of India and South Africa, has been adduced as
further evidence of this connection. But there are also genera of
snakes, of insects, and of plants, common to Madagascar and South
America only, which have been held to necessitate a direct land
connection between these countries. These views evidently refute
themselves, because any such land connections must have led to a far
greater similarity in the productions of the several countries than
actually exists, and would besides render altogether inexplicable the
absence of all the chief types of African and Indian mammalia from
Madagascar, and its marvellous individuality in every department of the
organic world.[169]
_Powers of Dispersal as illustrated by Insular Organisms._
Having arrived at the conclusion that our existing oceans have remained
practically unaltered throughout the Tertiary and Secondary periods of
geology, and that the distribution of the mammalia is such as might
have been brought about by their known powers of dispersal, and by such
changes of land and sea as have probably or certainly occurred, we are,
of course, restricted to similar causes to explain the much wider and
sometimes more eccentric distribution of other classes of animals and of
plants. In doing so, we have to rely partly on direct evidence of
dispersal, afforded by the land organisms that have been observed far
out at sea, or which have taken refuge on ships, as well as by the
periodical visitants to remote islands; but very largely on indirect
evidence, afforded by the frequent presence of certain groups on remote
oceanic islands, which some ancestral forms must, therefore, have
reached by transmission across the ocean from distant lands.
_Birds._
These vary much in their powers of flight, and their capability of
traversing wide seas and oceans. Many swimming and wading birds can
continue long on the wing, fly swiftly, and have, besides, the power of
resting safely on the surface of the water. These would hardly be
limited by any width of ocean, except for the need of food; and many of
them, as the gulls, petrels, and divers, find abundance of food on the
surface of the sea itself. These groups have a wide distribution
_across_ the oceans; while waders--especially plovers, sandpipers,
snipes, and herons--are equally cosmopolitan, travelling _along_ the
coasts of all the continents, and across the narrow seas which separate
them. Many of these birds seem unaffected by climate, and as the
organisms on which they feed are equally abundant on arctic, temperate,
and tropical shores, there is hardly any limit to the range even of some
of the species.
Land-birds are much more restricted in their range, owing to their
usually limited powers of flight, their inability to rest on the surface
of the sea or to obtain food from it, and their greater specialisation,
which renders them less able to maintain themselves in the new countries
they may occasionally reach. Many of them are adapted to live only in
woods, or in marshes, or in deserts; they need particular kinds of food
or a limited range of temperature; and they are adapted to cope only
with the special enemies or the particular group of competitors among
which they have been developed. Such birds as these may pass again and
again to a new country, but are never able to establish themselves in
it; and it is this organic barrier, as it is termed, rather than any
physical barrier, which, in many cases, determines the presence of a
species in one area and its absence from another. We must always
remember, therefore, that, although the presence of a species in a
remote oceanic island clearly proves that its ancestors must at one time
have found their way there, the absence of a species does not prove the
contrary, since it also may have reached the island, but have been
unable to maintain itself, owing to the inorganic or organic conditions
not being suitable to it. This general principle applies to all classes
of organisms, and there are many striking illustrations of it. In the
Azores there are eighteen species of land-birds which are permanent
residents, but there are also several others which reach the islands
almost every year after great storms, but have never been able to
establish themselves. In Bermuda the facts are still more striking,
since there are only ten species of resident birds, while no less than
twenty other species of land-birds and more than a hundred species of
waders and aquatics are frequent visitors, often in great numbers, but
are never able to establish themselves. On the same principle we account
for the fact that, of the many continental insects and birds that have
been let loose, or have escaped from confinement, in this country,
hardly one has been able to maintain itself, and the same phenomenon is
still more striking in the case of plants. Of the thousands of hardy
plants which grow easily in our gardens, very few have ever run wild,
and when the experiment is purposely tried it invariably fails. Thus A.
de Candolle informs us that several botanists of Paris, Geneva, and
especially of Montpellier, have sown the seeds of many hundreds of
species of exotic hardy plants, in what appeared to be the most
favourable situations, but that in hardly a single case has any one of
them become naturalised.[170] Still more, then, in plants than in
animals the absence of a species does not prove that it has never
reached the locality, but merely that it has not been able to maintain
itself in competition with the native productions. In other cases, as
we have seen, facts of an exactly opposite nature occur. The rat, the
pig, and the rabbit, the water-cress, the clover, and many other plants,
when introduced into New Zealand, nourish exceedingly, and even
exterminate their native competitors; so that in these cases we may feel
sure that the species in question did not exist in New Zealand simply
because they had been unable to reach that country by their natural
means of dispersal. I will now give a few cases, in addition to those
recorded in my previous works, of birds and insects which have been
observed far from any land.
_Birds and Insects at Sea._
Captain D. Fullarton of the ship _Timaru_ recorded in his log the
occurrence of a great number of small land-birds about the ship on 15th
March 1886, when in Lat. 48° 31' N., Long. 8° 16' W. He says: "A great
many small land-birds about us; put about sixty into a coop, evidently
tired out." And two days later, 17th March, "Over fifty of the birds
cooped on 15th died, though fed. Sparrows, finches, water-wagtails, two
small birds, name unknown, one kind like a linnet, and a large bird like
a starling. In all there have been on board over seventy birds, besides
some that hovered about us for some time and then fell into the sea
exhausted." Easterly winds and severe weather were experienced at the
time.[171] The spot where this remarkable flight of birds was met with
is about 160 miles due west of Brest, and this is the least distance the
birds must have been carried. It is interesting to note that the
position of the ship is nearly in the line from the English and French
coasts to the Azores, where, after great storms, so many bird stragglers
arrive annually. These birds were probably blown out to sea during their
spring migration along the south coast of England to Wales and Ireland.
During the autumnal migration, however, great flocks of
birds--especially starlings, thrushes, and fieldfares--have been
observed every year flying out to sea from the west coast of Ireland,
almost the whole of which must perish. At the Nash Lighthouse, in the
Bristol Channel on the coast of Glamorganshire, an enormous number of
small birds were observed on 3d September, including nightjars,
buntings, white-throats, willow-wrens, cuckoos, house-sparrows, robins,
wheatears, and blackbirds. These had probably crossed from
Somersetshire, and had they been caught by a storm the larger portion of
them must have been blown out to sea.[172]
These facts enable us to account sufficiently well for the birds of
oceanic islands, the number and variety of which are seen to be
proportionate to their facilities for reaching the island and
maintaining themselves in it. Thus, though more birds yearly reach
Bermuda than the Azores, the number of residents in the latter islands
is much larger, due to the greater extent of the islands, their number,
and their more varied surface. In the Galapagos the land-birds are still
more numerous, due in part to their larger area and greater proximity to
the continent, but chiefly to the absence of storms, so that the birds
which originally reached the islands have remained long isolated and
have developed into many closely allied species adapted to the special
conditions. All the species of the Galapagos but one are peculiar to the
islands, while the Azores possess only one peculiar species, and Bermuda
none--a fact which is clearly due to the continual immigration of fresh
individuals keeping up the purity of the breed by intercrossing. In the
Sandwich Islands, which are extremely isolated, being more than 2000
miles from any continent or large island, we have a condition of things
similar to what prevails in the Galapagos, the land-birds, eighteen in
number, being all peculiar, and belonging, except one, to peculiar
genera. These birds have probably all descended from three or four
original types which reached the islands at some remote period, probably
by means of intervening islets that have since disappeared. In St.
Helena we have a degree of permanent isolation which has prevented any
land-birds from reaching the island; for although its distance from the
continent, 1100 miles, is not so great as in the case of the Sandwich
Islands, it is situated in an ocean almost entirely destitute of small
islands, while its position within the tropics renders it free from
violent storms. Neither is there, on the nearest part of the coast of
Africa, a perpetual stream of migrating birds like that which supplies
the innumerable stragglers which every year reach Bermuda and the
Azores.
_Insects._
Winged insects have been mainly dispersed in the same way as birds, by
their power of flight, aided by violent or long-continued winds. Being
so small, and of such low specific gravity, they are occasionally
carried to still greater distances; and thus no islands, however remote,
are altogether without them. The eggs of insects, being often deposited
in borings or in crevices of timber, may have been conveyed long
distances by floating trees, as may the larvae of those species which
feed on wood. Several cases have been published of insects coming on
board ships at great distances from land; and Darwin records having
caught a large grasshopper when the ship was 370 miles from the coast of
Africa, whence the insect had probably come.
In the _Entomologists' Monthly Magazine_ for June 1885, Mr. MacLachlan
has recorded the occurrence of a swarm of moths in the Atlantic ocean,
from the log of the ship _Pleione_. The vessel was homeward bound from
New Zealand, and in Lat. 6° 47' N., Long. 32° 50' W., hundreds of moths
appeared about the ship, settling in numbers on the spars and rigging.
The wind for four days previously had been very light from north,
north-west, or north-east, and sometimes calm. The north-east trade wind
occasionally extends to the ship's position at that time of year. The
captain adds that "frequently, in that part of the ocean, he has had
moths and butterflies come on board." The position is 960 miles
south-west of the Cape Verde Islands, and about 440 north-east of the
South American coast. The specimen preserved is Deiopeia pulchella, a
very common species in dry localities in the Eastern tropics, and rarely
found in Britain, but, Mr. MacLachlan thinks, not found in South
America. They must have come, therefore, from the Cape Verde Islands, or
from some parts of the African coast, and must have traversed about a
thousand miles of ocean with the assistance, no doubt, of a strong
north-east trade wind for a great part of the distance. In the British
Museum collection there is a specimen of the same moth caught at sea
during the voyage of the _Rattlesnake_, in Lat. 6° N., Long. 22-1/2°
W., being between the former position and Sierra Leone, thus rendering
it probable that the moths came from that part of the African coast, in
which case the swarm encountered by the _Pleione_ must have travelled
more than 1200 miles.
A similar case was recorded by Mr. F.A. Lucas in the American periodical
_Science_ of 8th April 1887. He states that in 1870 he met with numerous
moths of many species while at sea in the South Atlantic (Lat. 25° S.,
Long. 24° W.), about 1000 miles from the coast of Brazil. As this
position is just beyond the south-east trades, the insects may have been
brought from the land by a westerly gale. In the _Zoologist_ (1864, p.
8920) is the record of a small longicorn beetle which flew on board a
ship 500 miles off the west coast of Africa. Numerous other cases are
recorded of insects at less distances from land, and, taken in
connection with those already given, they are sufficient to show that
great numbers must be continually carried out to sea, and that
occasionally they are able to reach enormous distances. But the
reproductive powers of insects are so great that all we require, in
order to stock a remote island, is that some few specimens shall reach
it even once in a century, or once in a thousand years.
_Insects at great Altitudes._
Equally important is the proof we possess that insects are often carried
to great altitudes by upward currents of air. Humboldt noticed them up
to heights of 15,000 and 18,000 feet in South America, and Mr. Albert
Müller has collected many interesting cases of the same character in
Europe.[173] A moth (Plusia gamma) has been found on the summit of Mont
Blanc; small hymenoptera and moths have been seen on the Pyrenees at a
height of 11,000 feet, while numerous flies and beetles, some of
considerable size, have been caught on the glaciers and snow-fields of
various parts of the Alps. Upward currents of air, whirlwinds and
tornadoes, occur in all parts of the world, and large numbers of insects
are thus carried up into the higher regions of the atmosphere, where
they are liable to be caught by strong winds, and thus conveyed enormous
distances over seas or continents. With such powerful means of
dispersal the distribution of insects over the entire globe, and their
presence in the most remote oceanic islands, offer no difficulties.
_The Dispersal of Plants._
The dispersal of seeds is effected in a greater variety of ways than are
available in the case of any animals. Some fruits or seed-vessels, and
some seeds, will float for many weeks, and after immersion in salt water
for that period the seeds will often germinate. Extreme cases are the
double cocoa-nut of the Seychelles, which has been found on the coast of
Sumatra, about 3000 miles distant; the fruits of the Sapindus saponaria
(soap-berry), which has been brought to Bermuda by the Gulf Stream from
the West Indies, and has grown after a journey in the sea of about 1500
miles; and the West Indian bean, Entada scandens, which reached the
Azores from the West Indies, a distance of full 3000 miles, and
afterwards germinated at Kew. By these means we can account for the
similarity in the shore flora of the Malay Archipelago and most of the
islands of the Pacific; and from an examination of the fruits and seeds,
collected among drift during the voyage of the _Challenger_, Mr. Hemsley
has compiled a list of 121 species which are probably widely dispersed
by this means.
A still larger number of species owe their dispersal to birds in several
distinct ways. An immense number of fruits in all parts of the world are
devoured by birds, and have been attractively coloured (as we have
seen), in order to be so devoured, because the seeds pass through the
birds' bodies and germinate where they fall. We have seen how frequently
birds are forced by gales of wind across a wide expanse of ocean, and
thus seeds must be occasionally carried. It is a very suggestive fact,
that all the trees and shrubs in the Azores bear berries or small fruits
which are eaten by birds; while all those which bear larger fruits, or
are eaten chiefly by mammals--such as oaks, beeches, hazels, crabs,
etc.--are entirely wanting. Game-birds and waders often have portions of
mud attached to their feet, and Mr. Darwin has proved by experiment that
such mud frequently contains seeds. One partridge had such a quantity of
mud attached to its foot as to contain seeds from which eighty-two
plants germinated; this proves that a very small portion of mud may
serve to convey seeds, and such an occurrence repeated even at long
intervals may greatly aid in stocking remote islands with vegetation.
Many seeds also adhere to the feathers of birds, and thus, again, may be
conveyed as far as birds are ever carried. Dr. Guppy found a small hard
seed in the gizzard of a Cape Petrel, taken about 550 miles east of
Tristan da Cunha.
_Dispersal of Seeds by the Wind._
In the preceding cases we have been able to obtain direct evidence of
transportal; but although we know that many seeds are specially adapted
to be dispersed by the wind, we cannot obtain direct proof that they are
so carried for hundreds or thousands of miles across the sea, owing to
the difficulty of detecting single objects which are so small and
inconspicuous. It is probable, however, that the wind as an agent of
dispersal is really more effective than any of those we have hitherto
considered, because a very large number of plants have seeds which are
very small and light, and are often of such a form as to facilitate
aerial carriage for enormous distances. It is evident that such seeds
are especially liable to be transported by violent winds, because they
become ripe in autumn at the time when storms are most prevalent, while
they either lie upon the surface of the ground, or are disposed in dry
capsules on the plant ready to be blown away. If inorganic particles
comparable in weight, size, or form with such seeds are carried for
great distances, we may be sure that seeds will also be occasionally
carried in the same way. It will, therefore, be necessary to give a few
examples of wind-carriage of small objects.
On 27th July 1875 a remarkable shower of small pieces of hay occurred at
Monkstown, near Dublin. They appeared floating slowly down from a great
height, as if falling from a dark cloud which hung overhead. The pieces
picked up were wet, and varied from single blades of grass to tufts
weighing one or two ounces. A similar shower occurred a few days earlier
in Denbighshire, and was observed to travel in a direction contrary to
that of the wind in the lower atmosphere.[174] There is no evidence of
the distance from which the hay was brought, but as it had been carried
to a great height, it was in a position to be conveyed to almost any
distance by a violent wind, had such occurred at the time.
_Mineral Matter carried by the Wind._
The numerous cases of sand and volcanic dust being carried enormous
distances through the atmosphere sufficiently prove the importance of
wind as a carrier of solid matter, but unfortunately the matter
collected has not been hitherto examined with a view to determine the
maximum size and weight of the particles. A few facts, however, have
been kindly furnished me by Professor Judd, F.R.S. Some dust which fell
at Genoa on 15th October 1885, and was believed to have been brought
from the African desert, consisted of quartz, hornblende, and other
minerals, and contained particles having a diameter of 1/500 inch, each
weighing 1/200,000 grain. This dust had probably travelled over 600
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