A new perspective on eruption data completeness: insights from the First Recorded EruptionS in the Holocene (FRESH) database by Burgos, Vanesa, Jenkins, Susanna F., Bebbington, Mark, Newhall,Chris, Taisne, Benoit

“…Regional RCDs in the Common Era (CE) range from as recently as 1964 CE in the Indian Ocean (southern) to 200 CE in Middle East and Western Indian Ocean. …”
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Reconstructing hydroclimate changes over the past 2500 years using speleothems from Pyrenean caves (NE Spain) by M. Bartolomé, M. Bartolomé, M. Bartolomé, A. Moreno, C. Sancho, I. Cacho, H. Stoll, N. Haghipour, N. Haghipour, Á. Belmonte, C. Spötl, J. Hellstrom, R. L. Edwards, H. Cheng, H. Cheng, H. Cheng

“…<p>Reconstructing of past hydroclimates at regional scales during the Common Era (CE) is necessary to place the current warming in the context of natural climate variability. …”
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Multi-Proxy Paleoecological Reconstruction of Peatland Initiation, Development and Restoration in an Urban Area (Moscow, Russia) by Yuri A. Mazei, Andrey N. Tsyganov, Ekaterina G. Ershova, Natalia G. Mazei, Valery E. Pimenov, Elizaveta V. Kotlyarova, Natalia V. Kuzmenkova, Mikhail S. Paramonov, Artemii D. Chulei, Anastasiya D. Makarova, Ivan A. Zhirov, Anna A. Tsaregorodtseva, Marina V. Zhuravleva, Andrey V. Kitashov, Ping Ding, Stepan N. Kalmykov

“…Peatland development started around 2550 before the common era (BCE) as a waterlogged eutrophic birch forest (terrestrial paludification) surrounded by a broadleaf forest. …”
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Changes in the Tree-Ring Width-Derived Cumulative Normalized Difference Vegetation Index over Northeast China during 1825 to 2013 CE by Ruoshi Liu, Yi Song, Yu Liu, Xuxiang Li, Huiming Song, Changfeng Sun, Qiang Li, Qiufang Cai, Meng Ren, Lu Wang

“…On this basis, we designed a transfer function to reconstruct the <b>CNDVI_JJ</b> for the CW–DHM region from 1825 to 2013 CE (Common Era). During the last 189 years, there were 28 years with high <b>CNDVI_JJ</b> values, and another 28 years with low values. …”
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Early Holocene ice on the Begguya plateau (Mt. Hunter, Alaska) revealed by ice core ¹⁴C age constraints by L. Fang, L. Fang, T. M. Jenk, T. M. Jenk, D. Winski, K. Kreutz, H. L. Brooks, E. Erwin, E. Osterberg, S. Campbell, C. Wake, M. Schwikowski, M. Schwikowski, M. Schwikowski

“…<p>Investigating North Pacific climate variability during warm intervals prior to the Common Era can improve our understanding of the behavior of ocean–atmosphere teleconnections between low latitudes and the Arctic under future warming scenarios. …”
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Ocean kinetic energy and photosynthetic biomass are important drivers of planktonic foraminifera diversity in the Atlantic Ocean by Marta M. Rufino, Marta M. Rufino, Emilia Salgueiro, Emilia Salgueiro, Antje A. H. L. Voelker, Antje A. H. L. Voelker, Paulo S. Polito, Pedro A. Cermeño, Fatima Abrantes, Fatima Abrantes

“…To assess the anthropogenic effect on biodiversity, it is essential to understand the global diversity distribution of the major groups at the base of the food chain, ideally before global warming initiation (1850 Common Era CE). Since organisms in the plankton are highly interconnected and carbonate synthesizing species have a good preservation state in the Atlantic Ocean, the diversity distribution pattern of planktonic foraminifera from 1741 core-top surface sediment samples (expanded ForCenS database) provides a case study to comprehend centennial to decadal time-averaged diversity patterns at pre-1970 CE times, the tempo of the substantial increase in tropospheric warming. …”
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Hydroclimate variability of western Thailand during the last 1400 years by Chawchai, Sakonvan, Liu, Guangxin, Bissen, Raphael, Scholz, Denis, Riechelmann, Dana F. C., Vonhof, Hubert, Mertz-Kraus, Regina, Chiang, Hong-Wei, Tan, Liangcheng, Wang, Xianfeng

“…Here, we present a new multi-proxy (δ18O and δ13C values, trace element concentrations, and grayscale values) data set of stalagmite KPC1 from Khao Prae cave in western Thailand spanning the last 1400 years (500–1900 CE; the Common Era). These multi-proxy data reveal a high variability between the wet and dry periods during 500–850 CE and 1150–1300 CE, stable climate conditions during 850–1150 CE, and overall dry conditions since 1300 CE. …”
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Incorporating temporal and spatial variability of salt-marsh foraminifera into sea-level reconstructions by Walker, Jennifer S., Cahill, Niamh, Khan, Nicole S., Shaw, Timothy Adam, Barber, Don, Miller, Kenneth G., Kopp, Robert E., Horton, Benjamin Peter

“…Information about the temporal and spatial variability of modern foraminiferal distributions was formally incorporated into the Bayesian transfer function through informative foraminifera variability priors and was applied to a Common Era relative sea-level record in New Jersey. …”
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MOLLA SABİR’İN KARDAŞLIK DERGİSİNDE TEFRİKA EDİLEN ‘KERKÜK ŞÂİRLERİ’ İSİMLİ ESERİ by Yağız YALÇINKAYA

“…He became one of the distinguished personalities of his period with his valuable works covering both the common era and the contemporary literary periods of the region, especially in Kirkuk, the city where he was born and lived. …”
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Improving the extraction of ancient Yersinia pestis genomes from the dental pulp by Pierre Clavel, Lexane Louis, Clio Der Sarkissian, Catherine Thèves, Claudia Gillet, Lorelei Chauvey, Gaétan Tressières, Stéphanie Schiavinato, Laure Calvière-Tonasso, Norbert Telmon, Benoît Clavel, Richard Jonvel, Stéfan Tzortzis, Laetitia Bouniol, Jean-Marc Fémolant, Jennifer Klunk, Hendrik Poinar, Michel Signoli, Caroline Costedoat, Maria A. Spyrou, Andaine Seguin-Orlando, Ludovic Orlando

“…Combining this procedure with DNA capture, we characterized the genome sequences of 12 ancient Y. pestis bacteria from France dating to the second pandemic outbreaks of the 17th and 18th centuries Common Era.…”
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A global compilation of diatom silica oxygen isotope records from lake sediment – trends and implications for climate reconstruction by P. Meister, A. Alexandre, H. Bailey, P. Barker, B. K. Biskaborn, E. Broadman, R. Cartier, R. Cartier, B. Chapligin, M. Couapel, J. R. Dean, B. Diekmann, B. Diekmann, P. Harding, P. Harding, A. C. G. Henderson, A. Hernandez, U. Herzschuh, U. Herzschuh, U. Herzschuh, S. S. Kostrova, J. Lacey, M. J. Leng, M. J. Leng, A. Lücke, A. W. Mackay, E. K. Magyari, B. Narancic, B. Narancic, C. Porchier, G. Rosqvist, A. Shemesh, C. Sonzogni, G. E. A. Swann, F. Sylvestre, H. Meyer

“…For mid- to high-latitude (<span class="inline-formula">&gt;</span> 45° N) lakes, we find common <span class="inline-formula"><i>δ</i>¹⁸O_BSi</span> patterns among the lake records during both the Holocene and Common Era (CE). These include maxima and minima corresponding to known climate episodes, such as the Holocene Thermal Maximum (HTM), Neoglacial Cooling, Medieval Climate Anomaly (MCA) and the Little Ice Age (LIA). …”
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