scholarly article | Q13442814 |
P356 | DOI | 10.1038/NGEO2652 |
P5875 | ResearchGate publication ID | 293640841 |
P50 | author | Jan Esper | Q6148878 |
Fredrik Charpentier Ljungqvist | Q22809975 | ||
Michael Sigl | Q42302355 | ||
Sebastian Wagner | Q57153146 | ||
Jed O. Kaplan | Q57178580 | ||
Vladimir Myglan | Q57913486 | ||
Lukas Wacker | Q57922757 | ||
Alexander Kirdyanov | Q58211505 | ||
Juerg Luterbacher | Q60667940 | ||
Michael McCormick | Q63208407 | ||
Paul J Krusic | Q63974951 | ||
Nicola Di Cosmo | Q64504131 | ||
Ulf Büntgen | Q67311305 | ||
Willy Tegel | Q67311434 | ||
Johann Jungclaus | Q98190218 | ||
P2093 | author name string | Michiel A. C. de Vaan | |
P2860 | cites work | Yersinia pestis DNA from skeletal remains from the 6(th) century AD reveals insights into Justinianic Plague | Q21089596 |
Climate-driven introduction of the Black Death and successive plague reintroductions into Europe | Q22248081 | ||
The Hot Summer of 2010: Redrawing the Temperature Record Map of Europe | Q24289126 | ||
Cultural responses to climate change during the late Holocene | Q28212564 | ||
Continental-scale temperature variability during the past two millennia | Q30049024 | ||
Timing and climate forcing of volcanic eruptions for the past 2,500 years. | Q30979223 | ||
Modeling the epidemiological history of plague in Central Asia: palaeoclimatic forcing on a disease system over the past millennium | Q30988256 | ||
2500 years of European climate variability and human susceptibility | Q33793030 | ||
1200 years of regular outbreaks in alpine insects. | Q51714464 | ||
Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea-ice/ocean feedbacks | Q55871065 | ||
Evaluation of climate models using palaeoclimatic data | Q56100241 | ||
Total solar irradiance during the Holocene | Q56609641 | ||
Robust global ocean cooling trend for the pre-industrial Common Era | Q56680688 | ||
Glacier dynamics, palaeohydrological changes and seismicity in southeastern Altai (Russia) and their influence on human occupation during the last 3000 years | Q57873429 | ||
Enhanced 20th-century heat transfer to the Arctic simulated in the context of climate variations over the last millennium | Q57892111 | ||
Climate Change during and after the Roman Empire: Reconstructing the Past from Scientific and Historical Evidence | Q60451071 | ||
Extraterrestrial confirmation of tree-ring dating | Q63972315 | ||
P433 | issue | 3 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | Little Ice Age | Q190530 |
P304 | page(s) | 231-236 | |
P577 | publication date | 2016-02-08 | |
P1433 | published in | Nature Geoscience | Q1337483 |
P1476 | title | Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD | |
P478 | volume | 9 |
Q104575000 | 20,000 years of societal vulnerability and adaptation to climate change in southwest Asia |
Q61443329 | 2600-years of stratospheric volcanism through sulfate isotopes |
Q60451068 | A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe |
Q114665316 | AD536 – Back to Nature? |
Q116259216 | All Change on the Land? Wheat and the Roman to Early Medieval Transition in England |
Q59197117 | Alpine ice-core evidence for the transformation of the European monetary system, AD 640–670 |
Q57892230 | Aromatic acids in a Eurasian Arctic ice core: a 2600-year proxy record of biomass burning |
Q114420346 | Bronze Age and Later Vegetation History on the Limestone Tabular Hills of North-East Yorkshire, UK: Pollen Diagrams from Dalby Forest |
Q58099909 | Challenges and perspectives for large-scale temperature reconstructions of the past two millennia |
Q36357213 | Changes in North Atlantic Oscillation drove Population Migrations and the Collapse of the Western Roman Empire. |
Q113303792 | Chinook Salmon, Late Holocene Climate Change, and the Occupational History of Kettle Falls, a Columbia River Fishing Station |
Q56001205 | Climate response to the Samalas volcanic eruption in 1257 revealed by proxy records |
Q89454796 | Climate stability and societal decline on the margins of the Byzantine empire in the Negev Desert |
Q31102498 | Climatic and environmental aspects of the Mongol withdrawal from Hungary in 1242 CE. |
Q110857763 | Cultural change and the climate record in final prehistoric and early medieval Ireland |
Q112750855 | Different Fates of Architectures |
Q57753686 | Does environmental archaeology need an ethical promise? |
Q58114216 | Dust clouds, climate change and coins: consiliences of palaeoclimate and economy in the Late Antique southern Levant |
Q56092781 | Evaluating the link between the sulfur-rich Laacher See volcanic eruption and the Younger Dryas climate anomaly |
Q57022725 | Evidence for magmatic carbon bias in C dating of the Taupo and other major eruptions |
Q46376521 | Evidence for very recent positive selection in Mongolians |
Q55411985 | Fen and Sea: Medieval and Early Modern Landscape Evolution in South-East Lincolnshire Before 1700 |
Q115040534 | Gregory of Tours on Sixth-Century Plague and Other Epidemics |
Q48120905 | Historical ecology reveals landscape transformation coincident with cultural development in central Italy since the Roman Period |
Q31157904 | Holocene peatland and ice-core data constraints on the timing and magnitude of CO2 emissions from past land use. |
Q46240535 | Improved recovery of ancient DNA from subfossil wood - application to the world's oldest Late Glacial pine forest |
Q117328032 | Isotopic insights into the early Medieval (600–1100 CE) diet in the Luistari cemetery at Eura, Finland |
Q64054883 | Limited capacity of tree growth to mitigate the global greenhouse effect under predicted warming |
Q33743512 | Microevolution of the noble crayfish (Astacus astacus) in the Southern Balkan Peninsula |
Q110245707 | Migration and cultural integration in the early medieval cemetery of Finglesham, Kent, through stable isotopes |
Q58080496 | Mild and Arid Climate in the Eastern Sahara-Arabian Desert During the Late Little Ice Age |
Q67224562 | No evidence for globally coherent warm and cold periods over the preindustrial Common Era |
Q47113694 | North Atlantic variability and its links to European climate over the last 3000 years |
Q57232368 | Out of Amazonia: Late-Holocene climate change and the Tupi–Guarani trans-continental expansion |
Q96765627 | Persistent warm Mediterranean surface waters during the Roman period |
Q119997090 | Plague, Climate and Faith in Early Medieval Western Britain: Investigating Narratives of Change |
Q42672688 | Q&A: What are pathogens, and what have they done to and for us? |
Q58175978 | Rapid transport of ash and sulfate from the 2011 Puyehue-Cordón Caulle (Chile) eruption to West Antarctica |
Q108081214 | Reccopolis revealed: the first geomagnetic mapping of the early medieval Visigothic royal town |
Q58058708 | Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks |
Q42371006 | Reply to 'Climate of doubt: a re-evaluation of Büntgen and Di Cosmo's environmental hypothesis for the Mongol withdrawal from Hungary, 1242 CE'. |
Q62268315 | Reply to 'Limited Late Antique cooling' |
Q47185020 | Scale-dependent climatic drivers of human epidemics in ancient China |
Q57802625 | Solar superstorm of AD 774 recorded subannually by Arctic tree rings |
Q115571544 | Something old, something new, something borrowed: New insights to human-environment interaction in medieval Novgorod inferred from tree rings |
Q58099903 | Temperature Covariance in Tree Ring Reconstructions and Model Simulations Over the Past Millennium |
Q112750814 | Terraced Fields, Irrigation Systems and Agricultural Production in Early Islamic Palestine and Jordan |
Q108888646 | The Colonisation of Uplands in Medieval Britain and Ireland: Climate, Agriculture and Environmental Adaptation |
Q87892764 | The Justinianic Plague: an interdisciplinary review |
Q99248414 | The potential of gypsum speleothems for paleoclimatology: application to the Iberian Roman Human Period |
Q117932502 | The role of drought during the Hunnic incursions into central-east Europe in the 4th and 5th c. CE |
Q59328842 | The timing and widespread effects of the largest Holocene volcanic eruption in Antarctica |
Q73249964 | The ‘Late Avar reform’ and the ‘long eighth century’: A tale of the hesitation between structural transformation and the persistent nomadic traditions (7th to 9th century AD) |
Q115011336 | Thirsty cities? The supply, management, and perception of water in Byzantine North Africa |
Q114030763 | Three Millennia of Vegetation, Land-Use, and Climate Change in SE Sicily |
Q28590670 | Three millennia of heavy rainfalls in Western Mediterranean: frequency, seasonality and atmospheric drivers |
Q57094208 | Tree rings reveal globally coherent signature of cosmogenic radiocarbon events in 774 and 993 CE |
Q48190351 | Volcanic dust veils from sixth century tree-ring isotopes linked to reduced irradiance, primary production and human health. |
Search more.