. The microscope and its revelations. slight grey colour, due proliaUv i The Depths of the Sea, y. no. s(.<- also //,if/r ,,i choUnnjo-, di. iii., andger Reports, e&peci&Ui Deep Sea Deposes (Murraj and MINUTE ORGANISMS AS ROCK-MAKERS I08; to the decomposing organic matter, becomes more pronounced, whileperfect shells of Globigerina almost disappear, fragments becomesmaller, and calcareous mud, structureless, and in a fine state ofdivision, is in greatly preponderating proportion. One can have nodoubt, on examining this sediment, that it is formed in the main bythe accumulation and disintegr

GLIX-115-2CF90JK

. The microscope and its revelations. slight grey colour, due proliaUv i The Depths of the Sea, y. no. s(.<- also //,if/r ,,i choUnnjo-, di. iii., andger Reports, e&peci&Ui Deep Sea Deposes (Murraj and MINUTE ORGANISMS AS ROCK-MAKERS I08; to the decomposing organic matter, becomes more pronounced, whileperfect shells of Globigerina almost disappear, fragments becomesmaller, and calcareous mud, structureless, and in a fine state ofdivision, is in greatly preponderating proportion. One can have nodoubt, on examining this sediment, that it is formed in the main bythe accumulation and disintegr
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. The microscope and its revelations. slight grey colour, due proliaUv i The Depths of the Sea, y. no. s(.<- also //,if/r ,,i choUnnjo-, di. iii., andger Reports, e&peci&Ui Deep Sea Deposes (Murraj and MINUTE ORGANISMS AS ROCK-MAKERS I08; to the decomposing organic matter, becomes more pronounced, whileperfect shells of Globigerina almost disappear, fragments becomesmaller, and calcareous mud, structureless, and in a fine state ofdivision, is in greatly preponderating proportion. One can have nodoubt, on examining this sediment, that it is formed in the main bythe accumulation and disintegr

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