Those dispatches converted the matter from a mere unusual incident
into something like a minor sensation. For, according to them, the
deposits of glistening gray slime had been left by the tides not only
along the Atlantic coast but along the Pacific also, and not only along
American shores but upon those of Europe and Asia and Africa, upon
all the shores of all earth's seas, in fact. Upon the jungle-bordered
beaches of the Philippines, and the cold gray Norwegian shores, and the
shelving sands of the Chilean coast, and the rocky cliffs of England,
the retreating tides had left the same thick coatings of jelly-like,
living slime. The phenomenon, whatever its cause, was world-wide,
as those morning dispatches showed, and because of that world-wide
scope was accorded a greatly increased space by the majority of that
morning's newspapers, seeming extraordinary enough to call for greater
attention. And even more extraordinary was it made, later in that day,
by the Barr-McMasters controversy concerning it, that acrid dispute of
scientists about the phenomenon's causes that stirred even the public
into a somewhat greater interest in it.
The controversy was precipitated, with surprizing abruptness, by the
statement made by Dr. Almeric Barr early on the 26th. It was toward Dr.
Barr, whose reputation among contemporary biologists was exceeded only
by that of the brilliant Dr. Herbert Munson of the Starford Foundation,
that the puzzled newspapers had turned when the glistening deposits
had first appeared at New York. They had brought him samples of the
stuff, asking his opinion of it, and his curiosity had been so stirred
that he had undertaken an analysis of it. It had proved, apparently, an
interesting enough analysis, for it was not until the next day that he
had given to the waiting journals any summary of it. When that summary
was published, though, appearing in the noon editions of that day's
papers, it proved a startling one.
Public-domain text, read in full here on John Shaqi.
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