ter age than the strata with corresponding
remains elsewhere; that in South America various species and genera of
men existed in tertiary times, some of them at least as advanced as
fairly well advanced modern savages; that there existed various land
bridges between South America and other southern continents, including
Africa; and that the ancestral types of modern mammals and of man
himself wandered across one of these bridges to the old world, and
that thence their remote descendants, after ages of time, returned to
the new. In addition to valuable investigations of fossil-bearing beds
in the Argentine, he made some excellent general suggestions, such as
that the pithecoid apes, like the baboons, do not stand in the line of
man's ancestral stem but represent a divergence from it away from
humanity and toward a retrogressive bestialization. But of his main
theses he proves none, and what evidence we have tells against them.
At the Museum of La Plata I found that the authorities were
practically a unit in regarding his remains of tertiary men and proto-
men as being either the remains of tertiary American monkeys or of
American Indians from strata that were long post-tertiary. The
extraordinary discovery, due to that eminent scientist and public
servant Doctor Moreno, of the remains of man associated with the
remains of the great extinct South American fauna, of the mylodon, of
a giant ungulate, of a huge cat like the lion, and of an extraordinary
aberrant horse (of a wholly different genus from the modern horse)
conclusively shows that in its later stages the South American fauna
consisted largely of types that elsewhere had already disappeared and
that these types persisted into what was geologically a very recent
period only some tens of thousands of years ago, when savage man of
practically a modern type had already appeared in South America. The
evidence we have, so far as it goes, tends to show that the South
American fauna always has been more archaic in type than the arctogeal
fauna of the same chronological level.
To loose generalizations, and to elaborate misinterpretations of
paleontological records, the kind of work done by Mr. Haseman
furnishes an invaluable antiscorbutic. To my mind, he has established
a stronger presumption in favor of the theory he champions than has
been established in favor of the theories of any of the learned and
able scientific men from whose conclusions he dissents. Further
rese
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