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NOTES ON RANGE IN DEPTH OF MARINE ALGjE. 149<br />

The influence of the law, that in water there is a limit of obliquity<br />

beyond which transmission into the air cannot occur, giving rise to<br />

total reflection, and the unequal absorption exerted on the different<br />

separable rays of light, can only be hinted at here in relation to this<br />

subject. According to Bouguer, sea-water at a depth of 700 feet loses<br />

all transparency. Mr. H. Wild, in a recent number of Poggendorff's<br />

' Annalen,' states that light, in traversing 5 metres in depth, has its<br />

intensity reduced to one-third. He, however, adds that the transpa-<br />

rency of water at low temperatures is greater than at higher.<br />

Further, it is very notable that in high northern latitudes, where<br />

thick ice covers the surface of the sea during great part of the year,<br />

and where, moreover, the absence of dii-ect sunlight for several mouths<br />

together produces very peculiar conditions, nevertheless seaweeds<br />

abound, the number of species not much more than fifty, but some of<br />

large size, and most of them individually plentiful.*<br />

The late Professor E. Porbes adopted the following zones in relation<br />

to the distribution of marine Organisms on the British shores :— 1st.<br />

Littoral zone, comprehending the space between tide marks. 2nd. The<br />

Laminarian, from low-water mark to 15 or 20 fathoms. 3rd. The Me-<br />

dian zone, f from 15 or 20 fathoms to 50. 4th. The Infra-median ; and<br />

5th. The Abyssal. In the first two of these seaweeds are abundant<br />

they are rare in the lower part of the median zone, and very rare indeed<br />

beyond it.<br />

In recording habitats of British Algce (as in ' Phycologia ' of the<br />

late Professor Harvey), the expression "cast up from deep water"<br />

is often used ; it is somewhat indefinite, nevertheless, as many delicate<br />

species are thrown on shore in very perfect condition,—they cannot<br />

have come from any great distance ; and if we examine the tidal chart<br />

in Johnston's ' Physical Atlas,' where depths round the British and<br />

Irish shores are also given, it will be seen that the line of 10 fathoms<br />

on the general coast is very narrow, but is wider in bays and arms of<br />

the sea ;<br />

and as these localities yield many species, 10 fathoms may be<br />

considered a common bathymetrical range. The following may be<br />

mentioned as reaching to or beyond 15 fathoms :<br />

—<br />

Chorda Filnm, Cul-<br />

ler ia hiuUifida, Zonaria parvula, Polysiphunia parasitica, Chylocludia<br />

* ' Journal of the Lhmean Society,' vol. ix.<br />

+ He used the term median or coralline zone, the latter very loose or incorrect<br />

if applied to the Corallinida of algologists.<br />

;

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