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Peruvian margin at 11° S, core 470-MUC29 (145 m)

Peruvian shelf and slope, Peru

Sediments

Type
Sediment

Multicorer from cruise M77/1 on the 11° S transect, Peruvian oxygen minimum zone. Pore waters are as heavy as or heavier than biogenic opal: precipitation of authigenic alumino-silicates about 2 ‰ lighter. Station coordinates not given in the article. Abundant opal (10 to 27 wt%). Site not precisely located: the source gives no coordinates.

δ30Si in ‰ (per mil) Values of the same system

Standard : NBS 28

ValueRangenMineral or matrixSource
1.23 ± 0.12 ‰1.09 / 1.41 ‰6pore water (0.2 µm filtered), dissolved silicon
Mean and standard deviation recalculated from 6 samples. Pore waters from 0 to 33 cm, Table 1.
Ehlert et al. (2016), Stable silicon isotope signatures of marine pore waters - Biogenic …
0.93 ± 0.17 ‰0.55 / 1.15 ‰12extracted biogenic opal (diatoms)
Mean and standard deviation recalculated from 12 samples. Biogenic opal from 0 to 48 cm, Table 1 (Modern Warm Period to Transition sediments).
Ehlert et al. (2016), Stable silicon isotope signatures of marine pore waters - Biogenic …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Peruvian margin at 11° S, core 470-MUC29 (145 m), isotope signatures. https://www.isofind.tech/isotopes/en/sites/marge-peruvienne-a-11-s-carotte-470-muc29-145-m/ (accessed 2026-10-13).

@misc{isofind2026peruvianmarginat11score470muc,
  title = {Peruvian margin at 11° S, core 470-MUC29 (145 m), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/marge-peruvienne-a-11-s-carotte-470-muc29-145-m/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13