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

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 9 de febrero de 2022

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Haeberli, Marcel, Daniel Baggenstos, Jochen Schmitt, et al. "Snapshots of mean ocean temperature over the last 700 000 years using noble gases in the EPICA Dome C ice core." Climate of the Past 17, no. 2 (2021): 843–67. http://dx.doi.org/10.5194/cp-17-843-2021.

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Abstract. Together with the latent heat stored in glacial ice sheets, the ocean heat uptake carries the lion's share of glacial–interglacial changes in the planetary heat content, but little direct information on the global mean ocean temperature (MOT) is available to constrain the ocean temperature response to glacial–interglacial climate perturbations. Using ratios of noble gases and molecular nitrogen trapped in the Antarctic EPICA Dome C ice core, we are able to reconstruct MOT for peak glacial and interglacial conditions during the last 700 000 years and explore the differences between th
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12

Voelker, A. H. L., T. Rodrigues, R. Stein, et al. "Variations in mid-latitude North Atlantic surface water properties during the mid-Brunhes: Does Marine Isotope Stage 11 stand out?" Climate of the Past Discussions 5, no. 3 (2009): 1553–607. http://dx.doi.org/10.5194/cpd-5-1553-2009.

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Abstract. New planktonic stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP Sites 1056/1058 and 980 to reconstruct hydrographic conditions during the middle Pleistocene spanning Marine Isotope Stages (MIS) 9–14 (300–540 ka). Together the study sites reflect western and eastern basin boundary currents as well as north to south transect sampling of subpolar and transitional water masses. Planktonic δ18O records indicate that during peak interglacial MIS 9 and 11 hydrographi
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13

CANDY, IAN, and ERIN L. MCCLYMONT. "Interglacial intensity in the North Atlantic over the last 800 000 years: investigating the complexity of the mid-Brunhes Event." Journal of Quaternary Science 28, no. 4 (2013): 343–48. http://dx.doi.org/10.1002/jqs.2632.

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14

Dupont, Lydie M., Thibaut Caley, and Isla S. Castañeda. "Effects of atmospheric CO<sub>2</sub> variability of the past 800 kyr on the biomes of southeast Africa." Climate of the Past 15, no. 3 (2019): 1083–97. http://dx.doi.org/10.5194/cp-15-1083-2019.

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Abstract. Very little is known about the impact of atmospheric carbon dioxide pressure (pCO2) on the shaping of biomes. The development of pCO2 throughout the Brunhes Chron may be considered a natural experiment to elucidate relationships between vegetation and pCO2. While the glacial periods show low to very low values (∼220 to ∼190 ppmv, respectively), the pCO2 levels of the interglacial periods vary from intermediate to relatively high (∼250 to more than 270 ppmv, respectively). To study the influence of pCO2 on the Pleistocene development of SE African vegetation, we used the pollen record
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15

Candy, Ian, and Montserrat Alonso-Garcia. "A 1 Ma sea surface temperature record from the North Atlantic and its implications for the early human occupation of Britain." Quaternary Research 90, no. 2 (2018): 406–17. http://dx.doi.org/10.1017/qua.2018.62.

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AbstractThe British Quaternary sequence has an exceptionally rich record of Palaeolithic archaeology up to 1 Ma. In this study, we reinvestigate foraminifera-based sea surface temperature (SST) reconstructions from the two marine core records (Ocean Drilling Program Site 980 and M23414) that are most relevant to the climatic history of the British Isles, consequently allowing the evolution of SST over the past 1 Ma to be studied. This is then compared with long-term changes with the British archaeological record in order to understand in greater detail the changing patterns of climatic forcing
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16

Huang, Huai‐Hsuan M., Moriaki Yasuhara, Hokuto Iwatani, Carlos A. Alvarez Zarikian, Maria‐Angela Bassetti, and Takuya Sagawa. "Benthic Biotic Response to Climate Changes Over the Last 700,000 Years in a Deep Marginal Sea: Impacts of Deoxygenation and the Mid‐Brunhes Event." Paleoceanography and Paleoclimatology 33, no. 7 (2018): 766–77. http://dx.doi.org/10.1029/2018pa003343.

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17

Huang, Huai-Hsuan May, Moriaki Yasuhara, Hokuto Iwatani, Tatsuhiko Yamaguchi, Katsura Yamada, and Briony Mamo. "Deep-sea ostracod faunal dynamics in a marginal sea: biotic response to oxygen variability and mid-Pleistocene global changes." Paleobiology 45, no. 1 (2018): 85–97. http://dx.doi.org/10.1017/pab.2018.37.

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AbstractDeep-sea benthic ostracod assemblages covering the last 2 Myr were investigated in Integrated Ocean Drilling Program Site U1426 (at 903 m water depth) in the southern Sea of Japan. Results show that (1) orbital-scale faunal variability has been influenced by eustatic sea-level fluctuations and oxygen variability and (2) secular-scale faunal transitions are likely associated with the mid-Brunhes event (MBE, ~0.43 Ma) and the onset of the Tsushima Warm Current (TWC, ~1.7 Ma).Krithe,Robertsonites, andAcanthocythereisare the three most abundant genera throughout the core, accounting for 78
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18

Chuey, John M., David K. Rea, and Nicklas G. Pisias. "Late Pleistocene Paleoclimatology of the Central Equatorial Pacific: A Quantitative Record of Eolian and Carbonate Deposition." Quaternary Research 28, no. 3 (1987): 323–39. http://dx.doi.org/10.1016/0033-5894(87)90001-9.

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AbstractDetailed records of δ18O, δ13C, percentage and mass accumulation rate of CaCO3, and eolian percentage, mass accumulation rate, and grainsize generated for core RC11-210 from the equatorial Pacific reveal the timing of paleoclimatic events over the past 950,000 yr. The CaCO3 percentage record shows the standard Pacific correlation of high CaCO3 content with glacial periods, but displays a marked change of character about 490,000 yr ago with older stages showing much less variability. The carbonate mass flux record, however, does not show such a noticeable change. Sedimentation rates var
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19

Kender, Sev, Adeyinka Aturamu, Jan Zalasiewicz, Michael A. Kaminski, and Mark Williams. "Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition." Journal of Micropalaeontology 38, no. 2 (2019): 177–87. http://dx.doi.org/10.5194/jm-38-177-2019.

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Abstract. The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but little is known of sea ice marginal locations such as the Bering Sea. The Bering Sea is the link between the Arctic and Pacific Ocean and is an area of high productivity and CO2 ventilation; it hosts a pronounced oxygen minimum zone (OMZ) and is thought to be the location of Glacial North Pacif
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20

Wang, PinXian, QianYu Li, Jun Tian, et al. "Long-term cycles in the carbon reservoir of the Quaternary ocean: a perspective from the South China Sea." National Science Review 1, no. 1 (2013): 119–43. http://dx.doi.org/10.1093/nsr/nwt028.

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Abstract In recent years, long-term, high-resolution records from the deep sea and ice-cores have offered new research opportunities for Quaternary science. Paleoclimate studies are no longer restricted to individual glacial cycles, but extend to long-term (≥105 yr) processes across those cycles. Ocean Drilling Program Leg 184 of the South China Sea in 1999 uncovered well-preserved sediment sections, in which three long-term cycles in Pleistocene carbon isotope (δ13C) sequence have been found and demonstrated to be common in the global ocean. Subsequent discoveries confirm the existence of lon
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21

Owen, R. Bernhart, Veronica M. Muiruri, Tim K. Lowenstein, et al. "Progressive aridification in East Africa over the last half million years and implications for human evolution." Proceedings of the National Academy of Sciences 115, no. 44 (2018): 11174–79. http://dx.doi.org/10.1073/pnas.1801357115.

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Evidence for Quaternary climate change in East Africa has been derived from outcrops on land and lake cores and from marine dust, leaf wax, and pollen records. These data have previously been used to evaluate the impact of climate change on hominin evolution, but correlations have proved to be difficult, given poor data continuity and the great distances between marine cores and terrestrial basins where fossil evidence is located. Here, we present continental coring evidence for progressive aridification since about 575 thousand years before present (ka), based on Lake Magadi (Kenya) sediments
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22

Bouttes, Nathaelle, Didier Swingedouw, Didier M. Roche, Maria F. Sanchez-Goni, and Xavier Crosta. "Response of the carbon cycle in an intermediate complexity model to the different climate configurations of the last nine interglacials." Climate of the Past 14, no. 2 (2018): 239–53. http://dx.doi.org/10.5194/cp-14-239-2018.

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Abstract. Atmospheric CO2 levels during interglacials prior to the Mid-Brunhes Event (MBE, ∼ 430 ka BP) were around 40 ppm lower than after the MBE. The reasons for this difference remain unclear. A recent hypothesis proposed that changes in oceanic circulation, in response to different external forcings before and after the MBE, might have increased the ocean carbon storage in pre-MBE interglacials, thus lowering atmospheric CO2. Nevertheless, no quantitative estimate of this hypothesis has been produced up to now. Here we use an intermediate complexity model including the carbon cycle to eva
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23

Cronin, T. M., G. S. Dwyer, E. K. Caverly, et al. "Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago." Scientific Reports 7, no. 1 (2017). http://dx.doi.org/10.1038/s41598-017-13821-2.

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