Records |
Author |
Priestley, K.; Debayle, E.; McKenzie, D.; Pilidou, S. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Upper mantle structure of eastern Asia from multimode surface waveform tomography |
Type |
Journal Article |
Year |
2006 |
Publication |
Journal of geophysical research-atmospheres |
Abbreviated Journal |
J. Geophys. Res. |
Volume |
111 |
Issue |
|
Pages |
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Keywords |
Asian upper mantle; multimode surface waveform; craton; 7208 Seismology: Mantle; 7218 Seismology: Lithosphere; 7255 Seismology: Surface waves and free oscillations; 7270 Seismology: Tomography |
Abstract |
We present a new three-dimensional Sv wave speed and azimuthal anisotropy model for the upper mantle of eastern Asia constrained by the analysis of more than 17,000 vertical component multimode Rayleigh wave seismograms. This data set allows us to build an upper mantle model for Asia with a horizontal resolution of a few hundred kilometers extending to ?400 km depth. At 75–100 km depth, there is approximately ±9% wave speed perturbation from the “smoothed PREM” reference model used in our analysis, and the pattern of azimuthal anisotropy is complex. Both the amplitude of the Sv wave speed heterogeneity and the complexity and amplitude of the azimuthal anisotropy decrease with depth. Above ?200 km depth the upper mantle structure of the model correlates with surface geology and tectonics; below ?200 km depth the structures primarily reflect the advection of material in the upper mantle. Since shear wave speed is principally controlled by temperature rather than by composition, Vs(z) can be used to calculate the temperature T(z), and hence map the lithospheric thickness. We use the relationship of Priestley and McKenzie to produce a contour map of the lithospheric thickness of eastern Asia from the surface wave tomography. This shows an extensive region of thick lithosphere beneath the Siberian Platform and the West Siberian Basin that extends to the European Platform, forming the stable Eurasian craton or core. The eastern portion of the Eurasian craton has controlled the geometry of continental deformation and the distribution of kimberlites in eastern Asia. |
Programme |
133 |
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Publisher |
American Geophysical Union |
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ISSN |
0148-0227 |
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Notes |
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Approved |
yes |
Call Number |
IPEV @ Thierry.Lemaire @ |
Serial |
5538 |
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Author |
Merrer, S.; Cara, M.; Rivera, L.; Ritsema, J. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Upper mantle structure beneath continents: New constraints from multi-mode Rayleigh wave data in western North America and southern Africa |
Type |
Journal Article |
Year |
2007 |
Publication |
Geophysical research letters |
Abbreviated Journal |
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Volume |
34 |
Issue |
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Pages |
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Keywords |
Rayleigh waves; upper mantle; 7208 Seismology: Mantle; 7255 Seismology: Surface waves and free oscillations; 7290 Seismology: Computational seismology |
Abstract |
We estimate the averaged 1-D shear-wave velocity of the upper mantle beneath western North America and the Kaapvaal region in southern Africa by inverting dispersion measurements of fundamental and higher Rayleigh modes recorded by ?2000 km aperture broadband arrays. The overtones at periods exceeding 25 s constrain the averaged 1-D shear-wave velocity to 650 km depth across the regional arrays. Our overtone analysis confirms the shear-wave velocity differences observed in global tomographic models with similar horizontal resolution: the western North American mantle features a prominent low velocity zone at depths 50–200 km, while the shear velocity in the upper 180–200 km of the mantle beneath southern Africa is at least 6% higher than in western North America which we interpret as the expression of a cratonic keel. There is no resolvable difference in shear-wave velocity between southern Africa and western North America below a depth of about 300 km. |
Programme |
133;906 |
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American Geophysical Union |
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ISSN |
0094-8276 |
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Approved |
yes |
Call Number |
IPEV @ Thierry.Lemaire @ |
Serial |
5540 |
Permanent link to this record |
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Author |
Pilidou, S., K.Priestley, O.Gudmundsson & E. Debayle |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Upper mantle S-wave speed heterogeneity beneath the North Atlantic and the surrounding region from regional surface wave tomography |
Type |
Journal Article |
Year |
2004 |
Publication |
Geophysical journal international |
Abbreviated Journal |
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Volume |
159 |
Issue |
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Pages |
1057-1076 |
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133;906 |
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ISSN |
0956-540X |
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Approved |
yes |
Call Number |
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Serial |
3360 |
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Author |
Debayle E. & Levêque J.J. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Upper mantle heterogeneities in the Indian ocean from waveform inversion. |
Type |
Journal Article |
Year |
1997 |
Publication |
Geophysical research letters |
Abbreviated Journal |
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Volume |
24 |
Issue |
3 |
Pages |
245-248 |
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Abstract |
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Programme |
133 |
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ISSN |
0094-8276 |
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Approved |
yes |
Call Number |
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Serial |
654 |
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Author |
Heintz M., Debayle E. & Vauchez A. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Upper mante structure of the South American continent and neighboring oceans from surface wave tomography |
Type |
Journal Article |
Year |
2005 |
Publication |
Tectonophysics |
Abbreviated Journal |
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Volume |
406 |
Issue |
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Pages |
115-139 |
Keywords |
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Abstract |
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Programme |
133;906 |
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ISSN |
0040-1951 |
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Approved |
yes |
Call Number |
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Serial |
3363 |
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Author |
A. Baranov, R. Tenzer, A. Morelli |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Updated Antarctic crustal model |
Type |
Journal |
Year |
2021 |
Publication |
Gondwana Research |
Abbreviated Journal |
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Volume |
89 |
Issue |
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Pages |
1-18 |
Keywords |
Antarctica Crustal structure Gondwana Sediments |
Abstract |
We use seismic data together with a subglacial bedrock relief from the BEDMAP2 database to obtain a new three-layer model of the consolidated (crystalline) crust of Antarctica that locally improves the global seismic crustal model CRUST1.0. We collect suitable data for constructing crustal layers, analyse them and build maps of the crustal layer thickness and seismic velocities. We use the subglacial relief according to a tectonic configuration and then interpolate data using a statistical kriging method. The P-wave velocity information from old seismic profiles have been supplemented with the new shear-wave velocity models. We adjust the thickness of crustal layers by multiplying a total crustal thickness by a percentage ratio of each individual layer at each point. Our results reveal large variations in seismic velocities between different crustal blocks forming Antarctica. The most pronounced differences exist between East and West Antarctica. In East Antarctica, a high P-wave velocity (vP > 7 km/s) layer in the lower crust is absent. The P-wave velocity in the lower crust changes from 6.1 km/s beneath the Lambert Rift to 6.9 km/s beneath the Wilkes Basin. In West Antarctica, a thick mafic lower crust is characterized by large P-wave velocities, ranging from 7.0 km/s under the Ross Sea to 7.3 km/s under the Byrd Basin. In contrast, velocities in the lower crust beneath the Transantarctic and Ellsworth-Whitmore Mountains are ~6.8 km/s. The P-wave velocities in the upper crust in East Antarctica are within the range 5.5–6.4 km/s. The upper crust of West Antarctica is characterized by the P-wave velocities of 5.6–6.3 km/s. The P-wave velocities in the middle crust vary within 5.9–6.6 km/s in East Antarctica and within 6.3–6.5 km/s in West Antarctica. A low-velocity layer (5.8–5.9 km/s) is detected at depth of ~20–25 km beneath the Princes Elizabeth Land. |
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133 |
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1342-937X |
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yes |
Call Number |
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Serial |
7994 |
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Author |
Garnier A, Chapuis J-L, Svanella-Dumas L, Renault D, Lebouvier M |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Update of the number and spread of alien plants in the French sub-Antarctic islands. XIth SCAR International Biology Symposium, Barcelone, Spain, 15-19/07/2013 |
Type |
Conference - International - Communication |
Year |
2013 |
Publication |
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136 |
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yes |
Call Number |
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Serial |
4356 |
Permanent link to this record |
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Author |
Guillaume Schwob, Léa Cabrol, Thomas Saucède, Karin Gérard, Elie Poulin, Julieta Orlando |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Unveiling the co-phylogeny signal between plunderfish Harpagifer spp. and their gut microbiomes across the Southern Ocean |
Type |
Journal |
Year |
2023 |
Publication |
Biorxiv |
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Volume |
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Abstract |
Understanding the factors that sculpt fish gut microbiome is challenging, especially in natural populations characterized by high environmental and host genomic complexity. Yet, closely related hosts are valuable models for deciphering the contribution of host evolutionary history to microbiome assembly, through the underscoring of phylosymbiosis and co-phylogeny patterns. Here, we hypothesized that the recent allopatric speciation of Harpagifer across the Southern Ocean (1.2–0.8 Myr) will promote the detection of robust phylogenetic congruence between the host and its microbiome. We characterized the gut mucosa microbiome of 77 individuals from four field-collected species of the plunderfish Harpagifer (Teleostei, Notothenioidei), distributed across three biogeographic regions of the Southern Ocean. We found that seawater physicochemical properties, host phylogeny and geography collectively explained 35% of the variation in bacterial community composition in Harpagifer gut mucosa. The core microbiome of Harpagifer spp. gut mucosa was characterized by a low diversity, mostly driven by selective processes, and dominated by a single Aliivibrio taxon detected in more than 80% of the individuals. Almost half of the core microbiome taxa, including Aliivibrio, harbored co-phylogeny signal at microdiversity resolution with Harpagifer phylogeny. This suggests an intimate symbiotic relationship and a shared evolutionary history with Harpagifer. The robust phylosymbiosis signal emphasizes the relevance of the Harpagifer model to understanding the contribution of fish evolutionary history to the gut microbiome assembly. We propose that the recent allopatric speciation of Harpagifer across the Southern Ocean may have generated the diversification of Aliivibrio into patterns recapitulating the host phylogeny. Importance Although challenging to detect in wild populations, phylogenetic congruence between marine fish and its microbiome is critical, as it allows highlighting potential intimate associations between the hosts and ecologically relevant microbial symbionts.Through a natural system consisting of closely related fish species of the Southern Ocean, our study provides foundational information about the contribution of host evolutionary trajectory on gut microbiome assembly, that represents an important yet underappreciated driver of the global marine fish holobiont. Notably, we unveiled striking evidence of co-diversification between Harpagifer and its microbiome, demonstrating both phylosymbiosis of gut bacterial communities, and co-phylogeny of specific bacterial symbionts, in patterns that mirror the host diversification. Considering the increasing threats that fish species are facing in the Southern Ocean, understanding how the host evolutionary history could drive its microbial symbiont diversification represents a major challenge to better predict the consequences of environmental disturbances on microbiome and host fitness. |
Programme |
1044 |
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yes |
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Serial |
8685 |
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Author |
Stefanutti L., Morandi M., Del Guasta M. & Godin Sdavid C. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Unusual PSCs observed by LIDAR in Antarctica. |
Type |
Journal Article |
Year |
1994 |
Publication |
Geophysical research letters |
Abbreviated Journal |
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Volume |
17 |
Issue |
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Pages |
2377-2380 |
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209 |
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0094-8276 |
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yes |
Call Number |
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Serial |
618 |
Permanent link to this record |
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Author |
Grémillet D., Chauvin C., Wilson R.P., Le Maho Y. & Wanless S. |
Title ![sorted by Title field, descending order (down)](img/sort_desc.gif) |
Unusual feather structure allows partial plumage wettability in diving great cormorants |
Type |
Journal Article |
Year |
2005 |
Publication |
Journal of avian biology |
Abbreviated Journal |
J. Avian Biol. |
Volume |
36 |
Issue |
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Pages |
1-7 |
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388 |
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0908-8857 |
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yes |
Call Number |
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Serial |
3471 |
Permanent link to this record |