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  • 1
    Online Resource
    Online Resource
    Newark :American Geophysical Union,
    Keywords: Biodiversity -- Galapagos Islands. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (446 pages)
    Edition: 1st ed.
    ISBN: 9781118852569
    Series Statement: Geophysical Monograph Series ; v.204
    Language: English
    Note: Intro -- Geophysical Monograph Series -- Copyright -- Contents -- Contributors -- Foreword: Darwin's Perspective -- Foreword: The Galápagos as a Natural Laboratory -- References -- Acknowledgments -- Chapter 1 Introduction -- Chapter 2 Contrasting Volcanism in Hawai'i and the Galápagos -- 2.1. Introduction -- 2.2. Magma Supply -- 2.2.1. Competition for magma supply and interactions between volcanoes -- 2.2.2. Archipelago-scale magma supply -- 2.3. Magma Storage -- 2.3.1. Characteristics of magma storage -- 2.3.2. Magma storage beneath volcanic flanks -- 2.4. Volcano Morphology and Structure -- 2.4.1. Volcano shape -- 2.4.2. Pattern of eruptive fissures -- 2.4.3. Calderas -- 2.4.4. Intracaldera faulting -- 2.4.5. Flank instability -- 2.5. Volcanic Eruptions and Volcano Evolution -- 2.5.1. Eruption style -- 2.5.2. Volcano evolution -- 2.6. Conclusions -- 2.7. Acknowledgments -- References -- Chapter 3 Galápagos and Easter: A Tale of Two Hotspots -- 3.1. Introduction -- 3.2. The Galápagos Islands -- 3.3. Easter-Salas y Gómez Seamount Chain -- 3.4. Discussion -- 3.4.1. Plumes at the edges of the LLSVP -- 3.4.2. Plume-Ridge Interaction Effects -- 3.4.3. Orientation of the chemical boundary -- 3.4.4. Geochemical heterogeneity of the Pacific LLSVP -- 3.5. Conclusions -- 3.6. Acknowledgments -- 3.7. Author Contributions -- References -- Chapter 4 Eruption Rates for Fernandina Volcano: A New Chronology at the Galápagos Hotspot Center -- 4.1. Introduction -- 4.2. Sampling and Analytical Details -- 4.3. Constraints on Flow Mapping -- 4.4. Eruption Rate Estimate from Young Flows -- 4.5. Age of Oldest Lava Flows -- 4.6. Magmatic/Mantle Helium and Galápagos Geographic Variability -- 4.7. Conclusions -- 4.8. Acknowledgments -- References -- Chapter 5 Galápagos Magma Chambers -- 5.1. Introduction -- 5.2. Evidence from Volcanic History and Geomorphology. , 5.3. Evidence from Deformation and Gravity -- 5.4. Evidence from Magma Compositions and Crystals -- 5.5. Petrologic Monitoring of Eruptions -- 5.6. Summary of Interpretations -- 5.7. An Evolutionary Model for Mushy Magma Chambers -- 5.8. Conclusions: the Dynamic and Thermal Evolution of Galápagos Magma Chambers -- 5.9. Acknowledgments -- References -- Chapter 6 The Geology and Geochemistry of Isla Floreana, Galápagos: A Different Type of Late-Stage Ocean Island Volcanism -- 6.1. Introduction -- 6.2. Geologic Background -- 6.3. Methods -- 6.4. Results -- 6.4.1. Geologic development of Floreana -- 6.4.2. Petrography of Floreana lavas -- 6.4.3. Mineral compositions -- 6.4.4. Major element compositions -- 6.4.5. Trace element compositions -- 6.4.6. Strontium, Neodymium, and Lead isotopic ratios -- 6.4.7. Age determinations -- 6.5. Discussion -- 6.5.1. Geologic development of Floreana -- 6.5.2. Petrogenetic model -- 6.5.3. The trace element composition of the Floreana ("FLO") component -- 6.5.4. Late-stage volcanism in Galápagos -- 6.6. Conclusions -- 6.7. Acknowledgments -- References -- Chapter 7 Plate Tectonics, Evolution, and the Survival of Species: A Modern Day Hotspot -- 7.1. Introduction -- 7.2. Tectonic Setting -- 7.2.1. General description -- 7.2.2. Age of Galápagos Islands and geographical relationship to plate motions -- 7.3. Fauna and Flora, and East-West Colonization -- 7.3.1. General description of life on oceanic islands -- 7.3.2. Life on Galápagos: ancient dating -- 7.3.3. Why east-to-west colonization? -- 7.4. Conclusion of Plate Motions Linked to Biodiversity Movements -- 7.4.1. New islands and the saving of native and endemic species -- 7.5. Volcanism Versus Introduced Species in the Survival of Species -- 7.6. Case Study of Fernandina: Haven or Hell? -- 7.6.1. General description. , 7.6.2. Conclusion of Fernandina as a Refuge of Galápagos Biodiversity -- 7.7. Biodiversity, Introduced Species, and Plate Tectonics -- 7.7.1. Contamination through introduced species -- 7.8. Fate of Biodiversity -- 7.9. Conclusions -- 7.10. Acknowledgments -- References -- Chapter 8 A Paleogeographic Model of the Galápagos Islands and Biogeographical and Evolutionary Implications -- 8.1. Introduction -- 8.2. Ages of Island Emergence -- 8.2.1. Plate tectonic estimates -- 8.2.2. Direct age measurements of lavas -- 8.2.3. New age determinations -- 8.3. Biological Implications of the Islands' Ages -- 8.3.1. General models of island biogeography -- 8.3.2. Testing the general dynamic model -- 8.3.3. Modifications to the general dynamic model -- 8.4. Movement and Subsidence of the Galápagos Islands -- 8.4.1. Subsidence model -- 8.4.2. Paleogeography of the pleistocene Galápagos -- 8.5. The Proto-Galápagos and Evolutionary Geographic Pathways -- 8.5.1. Implications for phylogenetic divergence -- 8.5.2. Comparison with phylogenetic estimates -- 8.5.3. The progression rule -- 8.5.4. Dispersal and vicariance -- 8.6. Conclusions -- 8.7. Appendix I: Emergence Ages of the Individual Galápagos Islands -- 8.7.1. Isla Fernandina -- 8.7.2. Isla Isabela -- 8.7.3. Isla Santiago -- 8.7.4. Isla Pinzón -- 8.7.5. Isla Rabida -- 8.7.6. Isla Santa Cruz -- 8.7.7. Isla Floreana -- 8.7.8. Isla Santa Fe -- 8.7.9. Isla San Cristóbal -- 8.7.10. Isla Española -- 8.7.11. Islas Genovesa, Pinta, and Marchena -- 8.7.12. Islas Wolf and Darwin -- 8.8. Acknowledgments -- References -- Chapter 9 Hydrogeology of the Galápagos Archipelago: An Integrated and Comparative Approach Between Islands -- 9.1. Introduction -- 9.2. Constraints of Basaltic Islands and Advocated Methodology -- 9.3. Main Features of San Cristóbal and Santa Cruz Islands and their Significance for Water Resources. , 9.3.1. Geology and weathering processes -- 9.3.2. Climate and water budget -- 9.3.3. Geomorphology and surface hydrology -- 9.3.4. Groundwater -- 9.4. Discussion -- 9.5. Recommendations for Groundwater Management Practices in the Galápagos -- 9.6. Acknowledgments -- References -- Chapter 10 Controls on the Hydrological and Topographic Evolution of Shield Volcanoes and Volcanic Ocean Islands -- 10.1. Introduction -- 10.2. A General Framework for Volcanic Landscape Evolution -- 10.3. Insights from a Global Compilation of Volcanic Ocean Islands and Shield Volcanoes -- 10.4. Phenomena Driving Landscape Evolution -- 10.4.1. Soil development and dust deposition set the stage for landscape dissection -- 10.4.2. Chemical and physical erosion rates change throughout landscape evolution -- 10.4.3. Precipitation rate affects erosion and soil development -- 10.4.4. Flank collapses can hasten topographic dissection -- 10.4.5. Volcanic architecture and tectonics constrain the patterns of landscape evolution -- 10.5. Other Controls on Volcanic Landscape Evolution -- 10.6. Conclusions -- 10.7. Acknowledgments -- References -- Chapter 11 Climate and the Global Reach of the Galápagos Archipelago: State of the Knowledge -- 11.1. Climatic and Oceanographic Setting -- 11.2. Influence on the Equilibrium State of the Tropical Pacific -- 11.2.1. Numerical modeling -- 11.2.2. Observations -- 11.2.3. Global climate modeling -- 11.3. Relationship with Climate Variability and Change -- 11.3.1. Islands in the crosshairs -- 11.3.2. Role in interannual climate variability (ENSO) -- 11.3.3. Role in anthropogenic climate change -- 11.4. Recap and Future Directions -- 11.5. Acknowledgments -- References -- Chapter 12 Assessment of the Chile 2010 and Japan 2011 Tsunami Events in the Galápagos Islands -- 12.1. Introduction -- 12.2. Background -- 12.3. Method of Analysis. , 12.4. Results -- 12.4.1. Tsunami Maule, Chile 2010 -- 12.4.2. Tsunami Tohoku, Japan 2011 -- 12.5. Discussion -- 12.6. Conclusions -- References -- Chapter 13 Patterns in Galápagos Magmatism Arising from the Upper Mantle Dynamics of Plume-Ridge Interaction -- 13.1. Introduction -- 13.2. Methods -- 13.2.1. Mantle convection -- 13.2.2. Model mantle heterogeneity, melting, and magma composition -- 13.3. Results: Predicted and Observed Magma Flux -- 13.3.1. Model 1: Plume with low viscosity, without a dependence on water content -- 13.3.2. Model 2: High viscosity in the shallowest upper mantle with the dependence on water content -- 13.4. Results: Predicted and Observed Magma Compositions -- 13.4.1. Model 1 geochemical variations -- 13.4.2. Model 2 geochemical variations -- 13.4.3. Along-axis variations in incompatible element concentration -- 13.5. Discussion -- 13.5.1. Model limitations and robustness of model results -- 13.5.2. The case for a low-viscosity Galápagos plume -- 13.5.3. The nature of heterogeneity in the Galápagos plume and ambient mantle -- 13.5.4. Incompatible element concentrations along the Galápagos Spreading Center -- 13.6. Conclusions -- 13.7. Acknowledgments -- References -- Chapter 14 Variations in Crustal Thickness, Plate Rigidity, and Volcanic Processes Throughout the Northern Galápagos Volcanic Province -- 14.1. Introduction -- 14.1.1. The mechanics of plume-ridge and plume-lithosphere interaction -- 14.1.2. Along- and off-axis expressions of the Galápagos mantle plume -- 14.2. Data -- 14.3. Gravity Anomalies -- 14.3.1. Free air anomaly -- 14.3.2. Mantle Bouguer Anomaly -- 14.3.3. Residual Mantle Bouguer Anomaly -- 14.4. Gravity-Derived Crustal Thickness Variations -- 14.4.1. Inversion of MBA for crustal thickness -- 14.4.2. Inversion results -- 14.4.3. Other contributions to the MBA. , 14.5. Plate Flexure Associated with the Galápagos Lineaments.
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  • 2
    ISSN: 1432-184X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Competition experiments were performed in a continuous-flow reactor using Methylosinus trichosporium OB3b, a type II methanotroph, and Methylomonas albus BG8, a type I methanotroph. The experiments were designed to establish conditions under which type II methanotrophs, which have significant cometabolic potential, prevail over type I strains. The primary determinants of species selection were dissolved methane, copper, and nitrate concentrations. Dissolved oxygen and methanol concentrations played secondary roles. M. trichosporium OB3b proved dominant under copper and nitratelimited conditions. The ratio of M. trichosporium to M. albus in the reactor increased ten-fold in less than 100 hours following the removal of copper from the reactor feed. Numbers of M. albus declined to levels that were below detection limits (〈106/ml) under nitrogen-limited conditions. In the latter experiment, the competitive success of M. trichosporiumdepended on the maintenance of an ambient dissolved oxygen level below about 7.5 × 10−5 M, or 30% of saturation with air. The ability of M. trichosporium to express soluble methane monooxygenase under copper limitation and nitrogenase under nitrate limitation was very significant. M. albus predominated under methane-limited conditions, especially when low levels of methanol were simultaneously added with methane to the reactor. The results imply that nitrogen limitation can be used to select for type II strains such as M. trichosporium OB3b.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1574-6968
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Soluble methane monooxygenase (sMMO) expression and activity were monitored under conditions that either promoted or suppressed the expression of nitrogenase in Methylosinus trichosporium OB3b wild-type (WT) and in its sMMO-constitutive mutant, PP319. Both WT and mutant cultures had reduced sMMO activity and protein levels under elevated O2 conditions (188 μM) compared with low O2 conditions (24 μM). Simultaneous N2 fixation also reduced sMMO activity in both cultures when O2 was low. However, when O2 levels were increased, nitrogenase expression ceased and sMMO activity was reduced by ∼77% in the WT, whereas sMMO and nitrogenase expression and activity in PP319 were relatively unaffected by the higher O2 levels. Western immunoblot analysis showed that the nitrogenase Fe protein resolved as two components (apparent molecular mass of 30.5 and 32 kDa) in both the WT and PP319 when O2 levels were low. When O2 levels were high, only the 32-kDa form of the Fe protein was present in PP319, whereas neither form was detectable in the WT. Aerotolerant N2 fixation appears to be associated with the 32-kDa Fe protein in M. trichosporium OB3b.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 433 (2005), S. 25-26 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A record of Earth's formation and its evolutionary history during the past 4,500 million years is preserved within the chemical and isotopic composition of the mantle. Fluids and the magmas expelled at the Earth's surface as basalt rocks provide samples for deciphering this record. In particular, ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. Fine-scale physical and chemical gradients and deep photosynthetic microbial populations were assessed to provide an initial characterisation of a small, thermally stratified reservoir (Cross Reservoir, Kansas, U.S.A.) and its deep chlorophyll maxima (DCM). Factors were identified that may affect vertical positioning of subepilimnetic photosynthetic sulphur bacteria (PSB) in lakes.2. Results indicate that Cross Reservoir is a mesotrophic, dimictic lake with large subepilimnetic chlorophyll maxima containing dense layers of PSB. Characteristics of the deep PSB community of Cross Reservoir strongly correlate with both light and nutrient gradients.3. The deep bacterial community mostly contained single-celled and aggregating green sulphur bacteria, specifically free-living Chlorobium limicola and the conspicuous motile ectosymbiotic consortium known as ‘Chlorochromatium aggregatum’. The bacteria were within the anaerobic hypolimnion, beneath a metalimnetic plate of Cryptomonas spp. and within very low sulphide and light conditions [mean of 67 μgS L−1 and 0.05% photosynthetically active radiation (PAR)]. Pigment concentrations and fluorescence trends indicate that the bacteria made up a larger proportion of the DCM biomass than did phytoplankton in 1996.4. Cross Reservoir shares characteristics with natural lakes world-wide that also include a deep PSB community containing dense layers of ‘C. aggregatum’. Correlation analyses indicate that PSB community positioning and density are related to light, sulphide supply, redox potentials and pH. A 2-factor principal components analysis (PCA) and other data trends supported these interpretations and indicated that PSB are sensitive to the thermal stability of the water column, are nitrogen limited and regulated more by sulphide or sulphide to light ratios than local levels of light. The sensitivity of these deep photosynthetic bacteria to environmental gradients, and their significance to some aquatic systems, demonstrate their potential as indicators of environmental disturbance.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Sudden exposure of an aquatic system to an insecticide can have significant effects on populations other than susceptible organisms. Although this is intuitively obvious, little is actually known about how such exposure might affect bacterial communities and their relative metabolic activity in ecosystems. Here, we assessed small sub-unit (ssu)-RNA levels in open and shaded 9 m3 aquatic mesocosms (16 units – 2 × 2 factorial design in quadruplicate) to examine the effects of sudden addition of deltamethrin to the units. When deltamethrin was added, a cascade of bacterial then phytoplankton “blooms” occurred over time. The bacterial bloom, which most likely included organisms from the plastid/cyanobacterial phylogenetic guild, was almost immediate (within hours), whereas the phytoplankton (algal) bloom lagged by about 4 days. This sequential response can be explained by an apparent sudden release of nutrients consequent to arthropod death that triggered a series of responses in the microbial loop. Interestingly, bacterial blooms were noted in both open and shaded mesocosms, whereas the algal bloom was only seen in open units, suggesting that both deltamethrin addition (and presumptive nutrient release) and an adequate light supply was required for the phytoplankton response. Overall, this work shows that microbial activities as reflected by ssu-rRNA levels can respond dramatically via apparently indirect effects following insecticide application.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Pb, Sr and Nd isotope variations are correlated in diverse lavas erupted at small seamounts near the East Pacific Rise. Tholeiites are isotopically indistinguishable from MORB (206Pb/204Pb=18.1–18.5; 87Sr/86Sr=0.7023–0.7028; 143Nd/144Nd=0.51326-0.51308); associated alkali basalts always show more radiogenic Pb and Sr signatures (206Pb/204Pb=18.8–19.2; 87Sr/86Sr=0.7029–0.7031) and less radiogenic Nd (143Nd/144Nd=0.51289–0.51301). The isotopic variability covers ∼80% of the variability for Pacific MORB, due to the presence of small-scale heterogeneity in the underlying mantle. Isotope compositions also correlate with trace element ratios such as La/Sm. Tholeiites at these seamounts have 3He/4He between 7.8–8.7 R A(R A= atmospheric ratio), also indistinguishable from MORB. He trapped in vesicles of alkali basalts, released by crushing in vacuo, has low 3He/4He (1.2–2.6 R)Ain conjunction with low helium concentrations ([He]〈5×10−8 ccSTP/g). In many cases post-eruptive radiogenic ingrowth has produced He isotope disequilibrium between vesicles and glass in the alkali basalts; subatmospheric 3He/4He ratios characterize the He dissolved in the glass which is released by melting the crushed powders. The narrow range of 3He/4He in the vesicles of the alkali basalts suggests that low 3He/4He is a source characteristic, but given their low [He] and high (U + Th), pre-eruptive radiogenic ingrowth cannot be excluded as a cause for low inherited 3He/4He ratios. Pb, Sr and Nd isotope compositions in lavas erupted at Shimada Seamount, an isolated volcano on 20 m.y. old seafloor at 17°N, are distinctly different from other seamounts in the East Pacific (206Pb/204Pb=18.8–19.0, 87Sr/ 86Sr≅0.7048 and 143Nd/144Nd≅0.51266). Relatively high 207Pb/204Pb (15.6–15.7) indicates ancient (〉2 Ga) isolation of the source from the depleted upper mantle, similar to Dupal components which are more prevalent in the southern hemisphere mantle. 3He/4He at Shimada Seamount is between 3.9–4.8 R A. Because the helium concentrations range up to 1.5×10−6, the low 3He/4He can not be due to radiogenic accumulation of 4He in the magma for reasonable volcanic evolution times. The low 3He/4He may be due to the presence of “enriched” domains within the lithosphere with high (U + Th)/He ratios, possibly formed during its accretion near the ridge. Alternatively, the low 3He/4He may be an inherent characteristic of an enriched component in the mantle beneath the East Pacific. Collectively, the He-Pb-Sr-Nd isotope systematics at East Pacific seamounts suggest that the range of isotope compositions present in the mantle is more readily sampled by seamount and island volcanism than by axial volcanism. Beneath thicker lithosphere away from the ridge axis, smaller degrees of melting in the source regions are less efficient in averaging the chemical characteristics of small-scale heterogeneities.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 326 (1987), S. 384-386 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A suite of basaltic glasses from small seamounts near the East Pacific Rise at 10-14° N has been analysed. This seamount field erupts chemically diverse lavas ranging from tholeiite (with mid-ocean-ridge basalt (MORE) chemistry) to alkali basalt (from a source with time-integrated higher Rb/Sr, ...
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1432-0819
    Keywords: Key words Hawaii ; Loihi ; Magmatic processes ; Submarine volcanism ; Petrology ; Geochronology ; Lava geochemistry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Samples of basalt were collected during the Rapid Response cruise to Loihi seamount from a breccia that was probably created by the July to August 1996 Loihi earthquake swarm, the largest swarm ever recorded from a Hawaiian volcano. 210Po–210Pb dating of two fresh lava blocks from this breccia indicates that they were erupted during the first half of 1996, making this the first documented historical eruption of Loihi. Sonobuoys deployed during the August 1996 cruise recorded popping noises north of the breccia site, indicating that the eruption may have been continuing during the swarm. All of the breccia lava fragments are tholeiitic, like the vast majority of Loihi's most recent lavas. Reverse zoning at the rim of clinopyroxene phenocrysts, and the presence of two chemically distinct olivine phenocryst populations, indicate that the magma for the lavas was mixed just prior to eruption. The trace element geochemistry of these lavas indicates there has been a reversal in Loihi's temporal geochemical trend. Although the new Loihi lavas are similar isotopically and geochemically to recent Kilauea lavas and the mantle conduits for these two volcanoes appear to converge at depth, distinct trace element ratios for their recent lavas preclude common parental magmas for these two active volcanoes. The mineralogy of Loihi's recent tholeiitic lavas signify that they crystallized at moderate depths (∼8–9 km) within the volcano, which is approximately 1 km below the hypocenters for earthquakes from the 1996 swarm. Taken together, the petrological and seismic evidence indicates that Loihi's current magma chamber is considerably deeper than the shallow magma chamber (∼3–4 km) in the adjoining active shield volcanoes.
    Type of Medium: Electronic Resource
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  • 10
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    Unknown
    Wiley
    In:  In: The Galápagos: A natural laboratory for Earth Sciences. , ed. by Harpp, K., Mittelstaedt, E., d'Ozouville, N. and Graham, D. W. AGU Geophysical Monograph, 204 . Wiley, Hoboken, NJ, pp. 393-414. ISBN 978-1-118-85241-5
    Publication Date: 2014-09-22
    Description: Along the Galápagos Spreading Center (GSC), 3He/4He varies from 8.5–5.9 RA. High 3He/4He ratios, resembling those in the western and southern Galápagos islands, are absent. This lack of high 3He/4He contrasts markedly with other localities of plume–ridge interaction, such as Iceland, Easter, and Amsterdam/St. Paul. The most striking feature is a 3He/4He gradient, decreasing westward from 8.4–7.0 RA between 89 and 93°W, where the GSC is shallowest and shows “axial high” morphology. The intra-segment 3He/4He variability within this region indicates that magma crosses the mantle/crust boundary at multiple points beneath individual ridge segments, and lateral mixing within the crust and upper mantle is limited. Some of the 3He/4He variability may also reflect transfer of discrete heterogeneity from beneath the northern sector of the Galápagos plateau. One possible explanation for the absence of high 3He/4He along the GSC is that helium is a relatively ineffective downstream tracer of mantle material from the core of the Galápagos plume, due to its preferential extraction beneath the archipelago compared to other incompatible, lithophile tracers. A second explanation is that the heterogeneous Galápagos plume is sheared in the upper mantle by motion of the Nazca Plate relative to the migrating GSC. In this case, plume core material having high 3He/4He (from beneath Fernandina and Isabela) would be dispersed mostly away from the ridge, while plume edge material having low 3He/4He plus enriched Sr and Pb isotope signatures (from beneath the northern periphery of the archipelago) is smeared into the sub-ridge mantle.
    Type: Book chapter , NonPeerReviewed
    Format: text
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