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201por Zeng, Weiping, Jiang, Haishui, Chen, Yan, Ogg, James, Zhang, Muhui, Dong, Hanxinshuo“…The Sevatian of the late Norian is one of the key intervals in biotic turnover and in changes of paleoclimate and paleoenvironments. Conodont faunas recovered from two sections of upper Norian strata of the Dashuitang and Nanshuba formations near Baoshan City in western Yunnan province provide new insights into the diversity and biostratigraphy of the Sevatian conodonts within China as well as globally. …”
Publicado 2023
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202“…We find remarkable consistency between paleotemperature proxies, theory, and climate model simulations of both LGM and future climates. Paleoclimate data thus provide crucial new support for TA, refining the range of future low-latitude, low-elevation TA to [Formula: see text] (95% confidence interval), i.e., land warming ~40% more than oceans. …”
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203por Walters, Andrew P., Tierney, Jessica E., Zhu, Jiang, Meyers, Stephen R., Graves, Katherine, Carroll, Alan R.“…To investigate hydroclimate variability in western North America during the EECO, we developed an orbitally resolved leaf wax δ(2)H record from one of the most well-dated terrestrial paleoclimate archives, the Green River Formation. Our δ(2)H(wax) results show ∼60‰ variation and evidence for eccentricity and precession forcing. iCESM simulations indicate that changes in the Earth’s orbit drive large seasonal variations in precipitation and δ(2)H of precipitation at our study site, primarily during the summer season. …”
Publicado 2023
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204“…Magnetic investigation of the 200 mm long sequoia material suggests that magnetic efficiency of natural remanence may be a sensitive paleoclimate indicator because it is substantially higher (in average >1%) during the Medieval Warm Epoch (700–1300 A.D.) than during the Little Ice Age (1300–1850 A.D.) where it is <1%. …”
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205Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Changepor Higuera, Philip E., Brubaker, Linda B., Anderson, Patricia M., Brown, Thomas A., Kennedy, Alison T., Hu, Feng Sheng“….; n = 44). Although paleoclimate interpretations and data from modern tundra fires suggest that increased burning was aided by low effective moisture, vegetation cover clearly played a critical role in facilitating the paleofires by creating an abundance of fine fuels. …”
Publicado 2008
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206por Cortés-Sánchez, Miguel, Morales-Muñiz, Arturo, Simón-Vallejo, María D., Lozano-Francisco, María C., Vera-Peláez, José L., Finlayson, Clive, Rodríguez-Vidal, Joaquín, Delgado-Huertas, Antonio, Jiménez-Espejo, Francisco J., Martínez-Ruiz, Francisca, Martínez-Aguirre, M. Aranzazu, Pascual-Granged, Arturo J., Bergadà-Zapata, M. Mercè, Gibaja-Bao, Juan F., Riquelme-Cantal, José A., López-Sáez, J. Antonio, Rodrigo-Gámiz, Marta, Sakai, Saburo, Sugisaki, Saiko, Finlayson, Geraldine, Fa, Darren A., Bicho, Nuno F.“…Obtained dates and paleoenvironmental records from the cave include isotopic, pollen, lithostratigraphic and sedimentological analyses and they are fully coherent with paleoclimate conditions expected for the different stages. …”
Publicado 2011
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207“…Furthermore, we provide a physiological foundation for the use of Brachystegia spiciformis tree-ring records in paleoclimate research.…”
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208por Robbins Schug, Gwen, Blevins, K. Elaine, Cox, Brett, Gray, Kelsey, Mushrif-Tripathy, V.“…The late mature phase (2200-1900 B.C.) was characterized by long-distance exchange networks, planned urban settlements, sanitation facilities, standardized weights and measures, and a sphere of influence over 1,000,000 square kilometers of territory. Recent paleoclimate reconstructions from the Beas River Valley demonstrate hydro-climatic stress due to a weakened monsoon system may have impacted urban centers like Harappa by the end of the third millennium B.C. the impact of environmental change was compounded by concurrent disruptions to the regional interaction sphere. …”
Publicado 2013
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209por Liu, Yi, Sun, Liguang, Zhou, Xin, Luo, Yuhan, Huang, Wen, Yang, Chengyun, Wang, Yuhong, Huang, Tao“…We present analyses of a lacustrine sediment core (DY6) on Dongdao Island, which provides high-resolution paleoclimate records for the South China Sea (SCS). Results of element analyses indicate that the concentrations of Ti and Al in DY6 are much higher than the background on the island. …”
Publicado 2014
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210por Gallagher, Kimberley L., Alfonso-Garcia, Alba, Sanchez, Jessica, Potma, Eric O., Santos, Guaciara M.“…This may have strong implications for understanding the mechanism of phytolith formation, and for use of phytolith carbon isotope values in dating or paleoclimate reconstruction.…”
Publicado 2015
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211por Zhang, Chunxia, Guo, Zhengtang, Deng, Chenglong, Ji, Xueping, Wu, Haibin, Paterson, Greig A., Chang, Lin, Li, Qin, Wu, Bailing, Zhu, Rixiang“…To understand the relationship between paleoclimate and hominoid evolution, we have studied sedimentary, clay mineralogy and geochemical proxies for the late Miocene STB section (~16 m thick; ca. 6.7–6.0 Ma). …”
Publicado 2016
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212“…Discriminating between black and white spruce (Picea mariana and Picea glauca) is a difficult palynological classification problem that, if solved, would provide valuable data for paleoclimate reconstructions. We developed an open-source visual recognition software (ARLO, Automated Recognition with Layered Optimization) capable of differentiating between these two species at an accuracy on par with human experts. …”
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213por Cotton, Jennifer M., Cerling, Thure E., Hoppe, Kathryn A., Mosier, Thomas M., Still, Christopher J.“…We apply this CART analysis to high-resolution gridded climate data and Coupled Model Intercomparison Project (CMIP5) mean paleoclimate model outputs to produce predictive isotope landscape models (“isoscapes”) for the current, mid-Holocene, and LGM average δ(13)C of grass-dominated areas across North America. …”
Publicado 2016
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214“…These results suggest that paleoclimate legacies supplement current climate in shaping phylogenetic patterns in North American trees, and especially so for gymnosperms.…”
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215“…These results provide important observational basis for the selection of appropriate downscaling strategies, deployment of climate-data collection networks, and interpreting paleoclimate reconstructions.…”
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216por Zhang, Ming-Li, Xiang, Xiao-Guo, Xue, Juan-Juan, Sanderson, Stewart C., Fritsch, Peter W.“…Based on an expanded data set of taxa and gene regions from those previously generated, we employed molecular clock and biogeographical analyses to infer the evolutionary history of Caragana and link it to floristic patterns, paleovegetation, and paleoclimate. Results indicate that Caragana is of arid origin from the Junggar steppe. …”
Publicado 2016
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217por Demény, Attila, Németh, Péter, Czuppon, György, Leél-Őssy, Szabolcs, Szabó, Máté, Judik, Katalin, Németh, Tibor, Stieber, József“…Speleothem deposits are among the most valuable continental formations in paleoclimate research, as they can be dated using absolute dating methods, and they also provide valuable climate proxies. …”
Publicado 2016
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218“…A third possibility is that both of these scenarios will play out simultaneously. We review paleoclimate evidence suggesting that (i) the middle latitudes were wetter during the last glacial maximum, (ii) a northward shift of the thermal equator attended the abrupt Bølling-Allerød climatic transition ~14.6 thousand years ago, and (iii) a southward shift occurred during the more recent Little Ice Age. …”
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219por Pausata, Francesco S. R., Zhang, Qiong, Muschitiello, Francesco, Lu, Zhengyao, Chafik, Léon, Niedermeyer, Eva M., Stager, J. Curt, Cobb, Kim M., Liu, Zhengyu“…In particular, a host of new paleoclimate records suggest that ENSO internal variability or other external forcings may have dwarfed the fairly modest ENSO response to precessional insolation changes simulated in climate models. …”
Publicado 2017
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220“…Our observations have implications to paleoclimate records utilizing this foundational foraminiferal species.…”
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