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with the MS., more or less fully.
Your doctrine of the cooling of the Tropics is a startling one, when
carried to the length of supporting plants of cold temperate regions;
and I must confess that, much as I should like it, I can hardly stomach
keeping the tropical genera alive in so very cool a greenhouse [pencil
note by C.D., "Not so very cool, but northern ones could range further
south if not opposed"]. Still I must confess that all your arguments pro
may be much stronger put than you have. I am more reconciled to iceberg
transport than I was, the more especially as I will give you any length
of time to keep vitality in ice, and more than that, will let you
transport roots that way also.

(333/1. The above letter was pinned to the following note by Mr.
Darwin.)

In answer to this show from similarity of American, and European and
Alpine-Arctic plants, that they have travelled enormously without any
change.

As sub-arctic, temperate and tropical are all slowly marching toward the
equator, the tropical will be first checked and distressed, similarly
(333/2. Almost illegible.) the temperate will invade...; after the
temperate can [not] advance or do not wish to advance further the
arctics will be checked and will invade. The temperates will have been
far longer in Tropics than sub-arctics. The sub-arctics will first have
to cross temperate [zone] and then Tropics. They would penetrate among
strangers, just like the many naturalised plants brought by man, from
some unknown advantage. But more, for nearly all have chance of doing
so.

(333/3. The point of view is more clearly given in the following
letters.)

LETTER 334. TO J.D. HOOKER. Down, November 15th [1856].

I shall not consider all your notes on my MS. for some weeks, till
I have done with crossing; but I have not been able to stop myself
meditating on your powerful objection to the mundane cold period (334/1.
See Letter 49.), viz. that MANY-fold more of the warm-temperate species
ought to have crossed the Tropics than of the sub-arctic forms. I really
think that to those who deny the modification of species this would
absolutely disprove my theory. But according to the notions which I am
testing--viz. that species do become changed, and that time is a most
important element (which I think I shall be able to show very clearly
in this case)--in such change, I think, the result would be as follows.
Some of the warm-temperate forms would penetrate the Tropics long before
the sub-arctic, and some might get across the equator long before the
sub-arctic forms could do so (i.e. always supposing that the cold came
on slowly), and therefore these must have been exposed to new associates
and new conditions much longer than the sub-arctic. Hence I should
infer that we ought to have in the warm-temperate S. hemisphere more
representative or modified forms, and fewer identical species than in
comparing the colder regions of the N. and S. I have expressed this
very obscurely, but you will understand, I think, what I mean. It is
a parallel case (but with a greater difference) to the species of the
mountains of S. Europe compared with the arctic plants, the S. European
alpine species having been isolated for a longer period than on the
arctic islands. Whether there are many tolerably close species in the
warm-temperate lands of the S. and N. I know not; as in La Plata, Cape
of Good Hope, and S. Australia compared to the North, I know not. I
presume it would be very difficult to test this, but perhaps you will
keep it a little before your mind, for your argument strikes me as
by far the most serious difficulty which has occurred to me. All your
criticisms and approvals are in simple truth invaluable to me. I fancy I
am right in speaking in this note of the species in common to N. and S.
as being rather sub-arctic than arctic.

This letter does not require any answer. I have written it to
ease myself, and to get you just to bear your argument, under the
modification point of view, in mind. I have had this morning a most
cruel stab in the side on my notion of the distribution of mammals in
relation to soundings.

LETTER 335. J.D. HOOKER TO CHARLES DARWIN. Kew, Sunday [November 1856].

I write only to say that I entirely appreciate your answer to my
objection on the score of the comparative rareness of Northern
warm-temperate forms in the Southern hemisphere. You certainly have
wriggled out of it by getting them more time to change, but as you must
admit that the distance traversed is not so great as the arctics have to
travel, and the extremes of modifying cause not so great as the arctics
undergo, the result should be considerably modified thereby. Thus: the
sub-arctics have (1) to travel twice as far, (2) taking twice the time,
(3) undergoing many more disturbing influences.

All this you have to meet by giving the North temperate forms simply
more time. I think this will hardly hold water.

LETTER 336. TO J.D. HOOKER. Down, November 18th [1856].

Many thanks for your note received this morning; and now for another
"wriggle." According to my notions, the sub-arctic species would advance
in a body, advancing so as to keep climate nearly the same; and as long
as they did this I do not believe there would be any tendency to change,
but only when the few got amongst foreign associates. When the tropical
species retreated as far as they could to the equator they would halt,
and then the confusion would spread back in the line of march from the
far north, and the strongest would struggle forward, etc., etc. (But
I am getting quite poetical in my wriggles). In short, I THINK the
warm-temperates would be exposed very much longer to those causes which
I believe are alone efficient in producing change than the sub-arctic;
but I must think more over this, and have a good wriggle. I cannot quite
agree with your proposition that because the sub-arctic have to travel
twice as far they would be more liable to change. Look at the two
journeys which the arctics have had from N. to S. and S. to N., with no
change, as may be inferred, if my doctrine is correct, from similarity
of arctic species in America and Europe and in the Alps. But I will not
weary you; but I really and truly think your last objection is not so
strong as it looks at first. You never make an objection without doing
me much good. Hurrah! a seed has just germinated after 21 1/2 hours in
owl's stomach. This, according to ornithologists' calculation, would
carry it God knows how many miles; but I think an owl really might go in
storm in this time 400 or 500 miles. Adios.

Owls and hawks have often been seen in mid-Atlantic.

(336/1. An interesting letter, dated November 23rd, 1856, occurs in the
"Life and Letters," II., page 86, which forms part of this discussion.
On page 87 the following passage occurs: "I shall have to discuss and
think more about your difficulty of the temperate and sub-arctic forms
in the S. hemisphere than I have yet done. But I am inclined to think
that I 

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