Literatura académica sobre el tema "Mid-Brunhes event"

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Artículos de revistas sobre el tema "Mid-Brunhes event"

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Holden, P. B., N. R. Edwards, E. W. Wolff, P. J. Valdes, and J. S. Singarayer. "The Mid-Brunhes Event and West Antarctic ice sheet stability." Journal of Quaternary Science 26, no. 5 (2011): 474–77. http://dx.doi.org/10.1002/jqs.1525.

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Blain, H. A., G. Cuenca-Bescos, I. Lozano-Fernandez, et al. "Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence." Geology 40, no. 11 (2012): 1051–54. http://dx.doi.org/10.1130/g33427.1.

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Barth, Aaron M., Peter U. Clark, Nicholas S. Bill, Feng He, and Nicklas G. Pisias. "Climate evolution across the Mid-Brunhes Transition." Climate of the Past 14, no. 12 (2018): 2071–87. http://dx.doi.org/10.5194/cp-14-2071-2018.

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Abstract. The Mid-Brunhes Transition (MBT) began ∼ 430 ka with an increase in the amplitude of the 100 kyr climate cycles of the past 800 000 years. The MBT has been identified in ice-core records, which indicate interglaciations became warmer with higher atmospheric CO2 levels after the MBT, and benthic oxygen isotope (δ18O) records, which suggest that post-MBT interglaciations had higher sea levels and warmer temperatures than pre-MBT interglaciations. It remains unclear, however, whether the MBT was a globally synchronous phenomenon that included other components of the climate system. Here
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Xu, Xinwen, Xiaoke Qiang, Sheng Hu, Hui Zhao, Chaofeng Fu, and Qing Zhao. "Records of the Mid-Brunhes Event in Chinese loess-paleosol sequences." Palaeogeography, Palaeoclimatology, Palaeoecology 543 (April 2020): 109596. http://dx.doi.org/10.1016/j.palaeo.2020.109596.

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Wang, Pinxian, Jun Tian, Xinrong Cheng, Chuanlian Liu, and Jian Xu. "Carbon reservoir changes preceded major ice-sheet expansion at the mid-Brunhes event." Geology 31, no. 3 (2003): 239. http://dx.doi.org/10.1130/0091-7613(2003)031<0239:crcpmi>2.0.co;2.

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JANSEN, J. H. F., A. KUIJPERS, and S. R. TROELSTRA. "A Mid-Brunhes Climatic Event: Long-Term Changes in Global Atmosphere and Ocean Circulation." Science 232, no. 4750 (1986): 619–22. http://dx.doi.org/10.1126/science.232.4750.619.

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Yin, Q. Z., and A. Berger. "Insolation and CO2 contribution to the interglacial climate before and after the Mid-Brunhes Event." Nature Geoscience 3, no. 4 (2010): 243–46. http://dx.doi.org/10.1038/ngeo771.

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Prokopenko, Alexander A., Eugene B. Karabanov, Douglas F. Williams, et al. "Biogenic Silica Record of the Lake Baikal Response to Climatic Forcing during the Brunhes." Quaternary Research 55, no. 2 (2001): 123–32. http://dx.doi.org/10.1006/qres.2000.2212.

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AbstractThis work presents a detailed, orbitally tuned biogenic silica record of continental paleoclimate change during the Brunhes chron. The Brunhes/Matuyama boundary lies within the warm isotopic stage 19 in Baikal, and the boundaries between eight lithological cycles correspond to terminations in the marine oxygen isotope record. The high amplitude and resolution of climatically driven changes in BioSi content in Lake Baikal sediments permits tuning of almost every precessional cycle during the Brunhes and reveals the structure of interglacial stages. For example, the last three interglaci
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Leonhardt, Adriana, Felipe A. L. Toledo, and João Carlos Coimbra. "The Mid-Brunhes event in the southwestern Atlantic Ocean: coccolithophore assemblages during the Mis 11-9." REVISTA BRASILEIRA DE PALEONTOLOGIA 18, no. 3 (2015): 343–54. http://dx.doi.org/10.4072/rbp.2015.3.01.

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Candy, I., G. R. Coope, J. R. Lee, et al. "Pronounced warmth during early Middle Pleistocene interglacials: Investigating the Mid-Brunhes Event in the British terrestrial sequence." Earth-Science Reviews 103, no. 3-4 (2010): 183–96. http://dx.doi.org/10.1016/j.earscirev.2010.09.007.

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Tesis sobre el tema "Mid-Brunhes event"

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Caley, Thibaut. "De l'importance de l'Océan Indien pour les paléoclimats quaternaires : la mousson et le courant des Aiguilles." Thesis, Bordeaux 1, 2011. http://www.theses.fr/2011BOR14331/document.

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L’océan Indien est le lieu de processus atmosphériques et océaniques majeurs dont les répercussions en terme climatique peuvent être de grandes importances. Cette thèse se propose de documenter les forçages, les variabilités, les impacts et les interactions de la mousson Indo-asiatique et du courant des Aiguilles à l’échelle orbitale (incluant les conditions glaciaires-interglaciaires) au cours de la période Quaternaire.Si le maximum d’insolation (minimum de précession et maximum d’obliquité) initie les fortes moussons Indo-asiatiques, des forçages internes au système climatique jouent égaleme
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Habicht, Mary Helen. "Examining the Mid- Brunhes Event in the Terrestrial Arctic: an Organic Geochemical Record from Lake El’gygytgyn, Russia." 2015. https://scholarworks.umass.edu/masters_theses_2/272.

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The characteristic glacial and interglacial cycles of the Pleistocene underwent a climatic transition at ~430 ka known as the Mid- Brunhes Event (MBE). Many studies, particularly from the Southern Hemisphere have noted that after this transition, the amplitude of the climatic cycles increased. Despite the indication of an MBE signal in many globally distributed paleoclimate records, the geographic extent of the climatic transition remains unknown and its presence in northern hemisphere and terrestrial records is debated. Lake El’gygytgyn is located in the far- east Russian Arctic and provides
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Actas de conferencias sobre el tema "Mid-Brunhes event"

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Jonas, A. S., M. A. C. Kars, T. Bauersachs, W. Rübsam, and L. Schwark. "Decoupling of Nw Pacific from Global Climate Evolution Linked to the Mid-Pleistocene Transition and Mid-Brunhes Event." In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201903064.

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Habicht, Helen, Isla Castañeda, Julie Brigham-Grette, Geoffrey Small, Julie Chessia, and Stephen Lukas. "SEARCHING FOR THE MID-BRUNHES EVENT IN THE TERRESTRIAL ARCTIC: AN ORGANIC GEOCHEMICAL PALEOCLIMATE RECORD FROM LAKE EL’GYGYTGYN, RUSSIA." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272102.

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