scholarly journals The isotopic composition of near-surface water vapor at the Maïdo observatory (Reunion Island, southwestern Indian Ocean) documents the controls of the humidity of the subtropical troposphere

2017 ◽  
Vol 122 (18) ◽  
pp. 9628-9650 ◽  
Author(s):  
Etienne Guilpart ◽  
Françoise Vimeux ◽  
Stéphanie Evan ◽  
Jérôme Brioude ◽  
Jean-Marc Metzger ◽  
...  
Keyword(s):  
Water Vapor ◽  
Surface Water ◽  
Indian Ocean ◽  
Isotopic Composition ◽  
Reunion Island ◽  
Near Surface ◽  
Réunion Island ◽  
Southwestern Indian Ocean

scholarly journals The epidemic of Dengue virus type-2 Cosmopolitan genotype on Reunion Island relates to its active circulation in the Southwestern Indian Ocean neighboring islands

Heliyon ◽  
2019 ◽  
Vol 5 (4) ◽  
pp. e01455 ◽  
Author(s):  
Hervé Pascalis ◽  
Jonathan Turpin ◽  
Marjolaine Roche ◽  
Pascale Krejbich ◽  
Gilles Gadea ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Dengue Virus ◽  
Virus Type ◽  
Reunion Island ◽  
Réunion Island ◽  
Dengue Virus Type 2 ◽  
Southwestern Indian Ocean

Morpho-molecular delineation of structurally important reef species, the fire corals, Millepora spp., at Réunion Island, Southwestern Indian Ocean

Hydrobiologia ◽  
2020 ◽  
Vol 847 (5) ◽  
pp. 1237-1255 ◽  
Author(s):  
E. Boissin ◽  
J. K. L. Leung ◽  
V. Denis ◽  
C. A. F. Bourmaud ◽  
N. Gravier-Bonnet
Keyword(s):  
Indian Ocean ◽  
Reunion Island ◽  
Réunion Island ◽  
Southwestern Indian Ocean

scholarly journals Unexplored Refugia with High Cover of Scleractinian Leptoseris spp. and Hydrocorals Stylaster flabelliformis at Lower Mesophotic Depths (75–100 m) on Lava Flows at Reunion Island (Southwestern Indian Ocean)

Diversity ◽  
2021 ◽  
Vol 13 (4) ◽  
pp. 141
Author(s):  
Ludovic Hoarau ◽  
Héloïse Rouzé ◽  
Émilie Boissin ◽  
Nicole Gravier-Bonnet ◽  
Patrick Plantard ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Lava Flows ◽  
Reunion Island ◽  
Mesophotic Coral Ecosystems ◽  
Réunion Island ◽  
Southwestern Indian Ocean

Despite increased attention over the last decade on Mesophotic Coral Ecosystems (MCEs) [...]

scholarly journals The mantle source of basalts from Reunion Island is not more oxidized than the MORB source mantle

2021 ◽  
Vol 177 (1) ◽  
Author(s):  
Maryjo Brounce ◽  
Edward Stolper ◽  
John Eiler
Keyword(s):  
Indian Ocean ◽  
Canary Islands ◽  
Mantle Source ◽  
Reunion Island ◽  
Near Surface ◽  
Isotopic Compositions ◽  
Mantle Sources ◽  
Réunion Island ◽  
Mantle Component ◽  
The Indian Ocean

AbstractGlasses quenched from relatively undegassed ocean island magmas erupted from volcanoes at Iceland, Hawaii, the Canary Islands, and Erebus have elevated Fe3+/∑Fe ratios compared to glasses quenched from mid-ocean ridge basalts. This has been ascribed to elevated fO2 of their mantle sources, plausibly due to subducted, oxidized near-surface-derived components in their mantle sources. The basaltic magmas from Reunion Island in the Indian ocean have Sr–Nd-Hf-Pb-Os isotopic compositions suggesting that their mantle sources contain little or no subducted near-surface materials and contain the C/FOZO/PREMA mantle component. To constrain the fO2 of the C/FOZO/PREMA mantle component and test the link between oxidized OIB and recycled surface-derived materials in their sources, we measured major and volatile element abundances and Fe3+/∑Fe ratios of naturally glassy, olivine-hosted melt inclusions from Piton de La Fournaise volcano, La Reunion. We conclude that the fO2 of the mantle source of these Reunion lavas is lower than of the mantle sources of primitive, undegassed magmas from Hawaii, Iceland, the Canary Islands, and Mt. Erebus, and indistinguishable from that of the Indian-ocean upper mantle. This finding is consistent with previous suggestions that the source of Reunion lavas (and the C/FOZO/PREMA mantle component) contains little or no recycled materials and with the suggestion that recycled oxidized materials contribute to the high fO2 of some other OIBs, especially those from incompatible-element-enriched mantle sources. Simple mixing models between oxidized melts of EM1 and HIMU components and relatively reduced melts of DMM can explain the isotopic compositions and Fe3+/∑Fe ratios of lavas from Hawaii, Iceland, the Canary Islands, and Mount Erebus; this model can be tested by study of additional OIB magmas, including those rich in the EM2 component.

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