Author
Listed:
- Jenna V. Adams
(University of California Santa Barbara)
- Matthew G. Jackson
(University of California Santa Barbara
University of California Santa Barbara, Department of Earth Science)
- Frank J. Spera
(University of California Santa Barbara)
- Allison A. Price
(University of California Santa Barbara)
- Benjamin L. Byerly
(University of California Santa Barbara
Thermo Fisher Scientific)
- Gareth Seward
(University of California Santa Barbara)
- John M. Cottle
(University of California Santa Barbara)
Abstract
Lavas erupted at hotspot volcanoes provide evidence of mantle heterogeneity. Samoan Island lavas with high 87Sr/86Sr (>0.706) typify a mantle source incorporating ancient subducted sediments. To further characterize this source, we target a single high 87Sr/86Sr lava from Savai’i Island, Samoa for detailed analyses of 87Sr/86Sr and 143Nd/144Nd isotopes and major and trace elements on individual magmatic clinopyroxenes. We show the clinopyroxenes exhibit a remarkable range of 87Sr/86Sr—including the highest observed in an oceanic hotspot lava—encompassing ~30% of the oceanic mantle’s total variability. These new isotopic data, data from other Samoan lavas, and magma mixing calculations are consistent with clinopyroxene 87Sr/86Sr variability resulting from magma mixing between a high silica, high 87Sr/86Sr (up to 0.7316) magma, and a low silica, low 87Sr/86Sr magma. Results provide insight into the composition of magmas derived from a sediment-infiltrated mantle source and document the fate of sediment recycled into Earth’s mantle.
Suggested Citation
Jenna V. Adams & Matthew G. Jackson & Frank J. Spera & Allison A. Price & Benjamin L. Byerly & Gareth Seward & John M. Cottle, 2021.
"Extreme isotopic heterogeneity in Samoan clinopyroxenes constrains sediment recycling,"
Nature Communications, Nature, vol. 12(1), pages 1-10, December.
Handle:
RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-21416-9
DOI: 10.1038/s41467-021-21416-9
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