Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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{{Recent Publications on Foraminifera Navigation}}<font size="2"> | {{Recent Publications on Foraminifera Navigation}}<font size="2"> | ||
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| + | ==LIVING BENTHIC FORAMINIFERA FROM THE CAP-FERRET CANYON: A COMPARISON BETWEEN THE CANYON AXIS AND THE SURROUNDING AREAS== | ||
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| + | [[Image:DeepSeaResearch_I_front.gif |left|80px|]]<font size="2"> | ||
| + | Living (Rose Bengal stained) benthic foraminiferal faunas were investigated at 13 deep-sea stations sampled in the Cap-Ferret Canyon area (NE Atlantic). One station (151 m) is located on the continental shelf close to the canyon head. All other stations are located along 2 bathymetric transects: 7 sites along the canyon axis with depths ranging from 300 to 3000 m and 5 stations along the adjacent flank with depths ranging from 300 m to 2000 m. ...... <br/> | ||
| + | '''Highlights''' | ||
| + | ► Live benthic foraminifera were studied at 13 stations in the Cap-Ferret Canyon. ► Fauna from the canyon axis were compared with live communities from adjacent areas. ► Geochemical data (e.g. OM composition) were used to described faunal distributions. ► Density and diversity along the canyon axis are higher than on the adjacent flank. ► This canyon shows lower density but higher diverse and complex fauna than Cap-Breton. | ||
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| + | <font size="2">([http://www.sciencedirect.com/science/article/pii/S0967063713000241 ABSTRACT]) | ||
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| + | ----Duros, P., Fontanier, C., Metzger, E., Cesbron, F., Deflandre, B., Schmidt, S., Buscail, R., Zaragosi, S., Kerhervé, P., Rigaud, S., Delgard, M.-L., Jorissen, F.J., in press. [http://www.sciencedirect.com/science/article/pii/S0967063713000241 Live (stained) benthic foraminifera from the Cap-Ferret Canyon (Bay of Biscay, NE Atlantic): A comparison between the canyon axis and the surrounding areas]. Deep Sea Research I, http://dx.doi.org/10.1016/j.dsr.2013.01.004 | ||
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==WESTERN PACIFIC THERMOCLINE STRUCTURE AND THE PACIFIC MARINE ITCZ DURING THE LGM== | ==WESTERN PACIFIC THERMOCLINE STRUCTURE AND THE PACIFIC MARINE ITCZ DURING THE LGM== | ||
