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Record #110477:

Laurentide ice extent inferred from stable isotopic composition (O,C) of ostracodes at Toronto, Canada / Henry P. Schwarcz, Nicholas Eyles.

Title: Laurentide ice extent inferred from stable isotopic composition (O,C) of ostracodes at Toronto, Canada / Henry P. Schwarcz, Nicholas Eyles.
Author(s): Schwarcz, Henry P.
Eyles, Nicholas.
Date: 1991.
In: Quaternary Research. (1991.), Vol. 35(3, Pt. 1) (1991)
Abstract: Presents data on isotopic composition of two species which differ in their ecological requirements and which were taken from stratigraphic sequence exposed along Scarborough Bluffs. Differences are reflected by differences in isotopic compositions and show they must have lived in different parts of glacial Lake Ontario. Co-occurrence in homogeneous samples of lake sediment indicates that post-mortem transport took place by means of sediment transport. Data suggest basin was fully glaciated only during Late Wisconsin.
Notes:

Quaternary Research. Vol. 35(3, Pt. 1) :305-320 (1991).

Keywords: 551.32 -- Glaciology.
551.336 -- Ice ages.
551.79 -- Quaternary.
551.33 -- Glacial geology.
551.332.2 -- Drift, glacial. Deposits.
54.027 -- Isotope analysis.
E7 -- Glaciology: glacial geology and ice ages.
(*41) -- Canada.
SPRI record no.: 110477

MARCXML

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005 20240414051749.0
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035 ## ‡aSPRI-110477
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSchwarcz, Henry P.
245 10 ‡aLaurentide ice extent inferred from stable isotopic composition (O,C) of ostracodes at Toronto, Canada /‡cHenry P. Schwarcz, Nicholas Eyles.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 305-320 :‡bdiags., tables, map.
500 ## ‡aQuaternary Research. Vol. 35(3, Pt. 1) :305-320 (1991).
520 3# ‡aPresents data on isotopic composition of two species which differ in their ecological requirements and which were taken from stratigraphic sequence exposed along Scarborough Bluffs. Differences are reflected by differences in isotopic compositions and show they must have lived in different parts of glacial Lake Ontario. Co-occurrence in homogeneous samples of lake sediment indicates that post-mortem transport took place by means of sediment transport. Data suggest basin was fully glaciated only during Late Wisconsin.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
700 1# ‡aEyles, Nicholas.
773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 35(3, Pt. 1) (1991) ‡wSPRI-46567
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240414