The Cambridge natural history, Vol. 03 (of 10)Cooke, A. H. (Alfred Hands)
Science
The Cambridge natural history, Vol. 03 (of 10)
Cooke, A. H. (Alfred Hands)
Animals
The land operculates give no help, and, of the carnivorous genera,
_Rhytida_ is a marked link between Africa and Australia, while
_Streptaxis_ is equally so between S. America and Africa. As regards
fresh-water Gasteropoda, _Ampullaria_ is common to S. America and
Africa, while _Isidora_ is common to Africa, Australia, and New
Zealand, but is altogether absent from S. America. _Gundlachia_ occurs
in Florida, Trinidad, and Tasmania, but has not been detected in
Africa. It must be concluded, therefore, that the present state of
the evidence which the Mollusca can afford, while exhibiting certain
curious points of relationship between the three regions in question,
is insufficient to warrant any decided conclusion.
[Illustration: FIG. 237.--_Macrocyclis laxata_ Fér., Chili.]
CHAPTER XII
DISTRIBUTION OF MARINE MOLLUSCA--DEEP-SEA MOLLUSCA
AND THEIR CHARACTERISTICS
Marine Mollusca may be divided roughly into Pelagic and non-Pelagic
genera. To the former division belong all Pteropoda and Heteropoda, and
a large number of Cephalopoda, together with a very few specialised
forms of Gasteropoda (_Ianthina_, _Litiopa_, _Phyllirrhoe_, etc.).
Pelagic Mollusca appear, as a rule, to live at varying depths below
the surface during the day, and to rise to the top only at night. The
majority inhabit warm or tropical seas, though some are exceedingly
abundant in the Arctic regions; _Clione_ and _Limacina_ have been
noticed as far north as 72°.[380]
The vertical range of Pelagic Mollusca has received attention from
Dr. Murray of the _Challenger_, Professor Agassiz of the _Blake_ and
_Albatross_, and others. Agassiz appears to have established the fact
that the surface fauna of the sea is limited to a comparatively narrow
belt of depth, and that there is no intermediate belt of animal life
between creatures which live on or near the bottom and the surface
fauna. Pelagic forms sink to avoid disturbances of various kinds,
to depths not much exceeding 150 to 200 fathoms, except in closed
seas like the Gulf of California and the Mediterranean, where the
bathymetrical range appears to be much greater.[381]
Non-Pelagic Mollusca are, from one point of view, conveniently
classified according to the different _zones of depth_ at which
they occur. Thus we are enabled to distinguish Mollusca of (_a_)
the _littoral_, (_b_) the _laminarian_, (_c_) the _nullipore_, or
_coralline_, and (_d_) the _abyssal_ zones. It must be borne in mind,
however, that these zones cannot be exactly defined, and that while the
littoral zone may be understood to imply the area between tide-marks,
and the abyssal zone a depth of 500 fathoms and upwards, the limits
between the laminarian and the coralline, and between the coralline and
abyssal zones can only be fixed approximately.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account