B. Ayling
The ocean's strontium
isotope composition has been changing through geologic time,
with intervals of both decreasing and increasing 87Sr /86Sr ratio
indicated by analysis of deep sea sediment cores. Since the mid-Cretaceous
(~100Ma), the general trend has been a gradual increase in the
87Sr /86Sr ratio from 0.70740 to its present day value of 0.70917.
The three main sources of strontium input into the oceans are
hydrothermal exchange at mid oceanic ridges, river runoff from
continental weathering, and release of strontium from the skeletons
of marine carbonates due to lowering of sea level and subsequent
carbonate exposure and recrystallisation. Mid oceanic ridge-derived
strontium typically displays a lower 87Sr /86Sr ratios of 0.703,
while river runoff is usually higher (around 0.711) due to weathering
of basement rocks which are relatively enriched in radiogenic
strontium. Carbonate weathering acts as a buffer to the ocean's
changing strontium isotope composition, as it negates the increasing
87Sr /86Sr ratio by contributing 87Sr /86Sr ratios from carbonates
formed when the ocean's 87Sr /86Sr was lower.
Because of these changes in marine 87Sr /86Sr,
strontium isotopes in fossil material have the potential to date
and/or correlate marine sequences. In addition, there has been
work into the utilisation of strontium isotopes as paleosalinity
indicators where d18O or
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d13C paleosalinity interpretations are questionable.
Strontium isotope ratios appear unaffected by biological processes
or evaporation, and are therefore more likely to remain conservative
in the seawater-freshwater mixing zone than d13C or d18O.
Part of my work will entail measurement of
strontium isotopes from Pliocene and Pleistocene marine molluscs
collected from the Wanganui Basin, New Zealand. The Wanganui
Basin contains a ca. 2km thick cyclothemic sedimentary sequence
which represents a near continuous record of predominantly marine
sediment deposition from the late Pliocene (ca.2.5 Ma) to late
Pleistocene. Mollusc samples were collected from 5 units which
are chronologically dispersed throughout the section. These are
the:
Landguard Formation (~0.25 Ma)
Tainui Shellbed (~0.5 Ma)
Kupe Formation (~0.68 Ma)
Omapu Shellbed (~0.85 Ma)
Hautawa Shellbed. (~2.5 Ma)
The ages of these deposits are already fairly
well constrained by the combination of cyclostratigraphy, tephrochronology,
biostratigraphy and paleomagnetic studies. It will therefore
be interesting to analyse strontium isotopes from these deposits
to provide additional age constraints/dating comparisons, and
potentially add more data to the Pleistocene section of the ocean's
strontium isotope evolution curve which is somewhat lacking in
detail.
Macrofossils from these units generally show
excellent preservation for the 4 youngest samples, particularly
the Tainui Shellbed (see Figure 3).
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