IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP

Reimer, Paula J.; Baillie, M. G. L.; Bard, Édouard; Bayliss, Alex; Beck, J. Warren; Blackwell, Paul G.; Ramsey, Christopher Bronk; Buck, Caitlin E.; Burr, George S.; Edwards, R. Lawrence; Friedrich, Michael; Grootes, P. M.; Guilderson, Thomas P.; Hajdas, Irka; Heaton, Timothy J; Hogg, Alan G.; Hughen, KA; Kaiser, Klaus Félix; Kromer, Bernd; McCormac, F. G.; Manning, Sturt W.; Reimer, Ron W; Richards, David A.; Southon, John; Talamo, Sahra; Turney, Chris; Plicht, Johannes van der; Weyhenmeyer, C. E.

doi:10.1017/s0033822200034202

Cited by 4,062 publications

(2,795 citation statements)

References 120 publications

Supporting

Mentioning

2,717

Contrasting

Unclassified

Order By: Relevance

“…Ten radiocarbon-based calendar age ranges for terrestrial plant fragments taken from MLT1 and five from MLT2 are plotted versus the depths from which they were collected in each core. Calendar ages and ranges in years before 1950 A.D. were found from 14C ages and uncertainties using the IntCal09 calibration dataset in the Calib6 program (Reimer et al 2009). See Tables 3 and 4 for details.…”

Section: Discussionmentioning

confidence: 99%

See 1 more Smart Citation

A decadally-resolved paleohurricane record archived in the late Holocene sediments of a Florida sinkhole

Lane¹,

Donnelly²,

Woodruff³

et al. 2011

Marine Geology

134

217

View full text Add to dashboard Cite

A 4500-year record of hurricane-induced storm surges is developed from sediment cores collected from a coastal sinkhole near Apalachee Bay, Florida. Recent deposition of sand layers in the upper sediments of the pond was found to be contemporaneous with significant, historic storm surges at the site modeled using SLOSH and the Best Track, post-1851 A.D. dataset. Using the historic portion of the record for calibration, paleohurricane deposits were identified by sand content and dated using radiocarbon-based age models. Marine-indicative foraminifera, some originating at least 5 km offshore, were present in several modern and ancient storm deposits. The presence and long-term preservation of offshore foraminifera suggest that this site and others like it may yield promising microfossil-based paleohurricane reconstructions in the future. Due to the sub-decadal (~ 7 year) resolution of the record and the site's high susceptibility to hurricane-generated storm surges, the average, local frequency of recorded events, approximately 3.9 storms per century, is greater than that of previously published paleohurricane records from the region. The high incidence of recorded events permitted a time series of local hurricane frequency during the last five millennia to be constructed. Variability in the frequency of the largest storm layers was found to be greater than what would likely occur by chance alone, with intervals of both anomalously high and low storm frequency identified. However, the rate at which smaller layers were deposited was relatively constant over the last five millennia. This may suggest that significant variability in hurricane frequency has occurred only in the highest magnitude events. The frequency of high magnitude events peaked near 6 storms per century between 2800 and 2300 years ago. High magnitude events were relatively rare with about 0-3 storms per century occurring between 1900 to 1600 years ago and between 400 to 150 years ago. A marked decline in the number of large storm deposits, which began around 600 years ago, has persisted through present with below average frequency over the last 150 years when compared to the preceding five millennia.

show abstract

Section: Discussionmentioning

confidence: 99%

“…Calendar ages (in years before present, where present is 1950 A.D. by convention) and corresponding uncertainties were calculated from 14 C ages and associated analytical errors using the IntCal09 calibration curves in the Calib6 program (Reimer et al 2009).…”

Section: Age Controlmentioning

confidence: 99%

A decadally-resolved paleohurricane record archived in the late Holocene sediments of a Florida sinkhole

Lane¹,

Donnelly²,

Woodruff³

et al. 2011

Marine Geology

134

217

View full text Add to dashboard Cite

show abstract

“…Os testemunhos foram coletados com aparelho Russian Peat Borer (Moore et al 1991) (Reimer et al 2009) apontando respectivamente 7.908±33 anos AP e 7.817±41 anos AP.…”

Section: Methodsunclassified

Grãos de pólen de angiospermas do Holoceno (7908±30 anos AP-atual) da Planície Costeira sul-catarinense, Brasil

2012

View full text Add to dashboard Cite

RESUMO(Grãos de pólen de angiospermas do Holoceno (7908±30 anos AP-atual) da Planície Costeira sul-catarinense, Brasil). Este trabalho apresenta as descrições palinotaxonômicas, a partir da análise palinológica de sedimentos de duas seções turfáceas na Planície Costeira sul do estado de Santa Catarina, nos municípios de Santa Rosa do Sul e São João do Sul. Uma amostra da porção basal dos testemunhos foi datada em ( 14 C) em 7908±33 anos AP para Santa Rosa do Sul e 7817±41 anos AP para São João do Sul, ambos referente ao Holoceno inferior. Foram descritos 62 tipos de grãos de pólen relacionados a 49 famílias de angiospermas atuais, que expressam diferentes habitats e hábitos ecoló-gicos. O presente trabalho juntamente com a primeira parte, que trata das descrições palinotaxonômicas de fungos, criptógamas e outros palinomorfos recuperados de sedimentos, contribui com o reconhecimento da vegetação que abrigava a Planície Costeira sul-catarinense, durante o Holoceno. As análises palinotaxonômicas constituem a base das interpretações paleoambientais e paleoclimáticas neste setor da costa brasileira. Palavras-chave:Descrições polínicas, Quaternário, Holoceno, Planície Costeira, Santa Catarina ABSTRACT (Catalogue of angiosperm pollen from Holocene sediments of the Coastal Plain, Santa Catarina, Brazil). This paper presents palinotaxonomic descriptions, from a pollen analysis of sediments from two cores taken from the southern Coastal Plain of Santa Catarina State (in the municipalities of Santa Rosa do Sul and São João do Sul). A basal sample from the Santa Rosa do Sul and São João do Sul had a 14 C age of 7908±33 and 7817±41 yr BP for the Lower Holocene, respectively. Sixty-two types of pollen grains were described from 49 angiosperm families, which are associated with different habitats and ecological habits. This work is published in association with Part I, which comprises palinotaxonomic descriptions of fungi, cryptogams and other palynomorphs recovered from the sediments, and contributes to the identification of vegetation that occurred on the Coastal Plain of southern Santa Catarina during the Holocene. Palinotaxonomic analyses form the basis of paleoclimatic and paleoenvironmental interpretations in this region of the Brazilian coast.

show abstract

“…Four sam ples were ex am ined with the AMS method in the Poznañ Ra dio car bon Lab o ra tory, whereas the other four sam ples were dated with the con ven tional method in the Ra diocar bon Lab o ra tory, Silesian Uni ver sity of Tech nol ogy at Gliwice (Po land). The ages were cal i brated with the OxCal v4.1.7 software (Reimer et al, 2009) to cal BP age (see Ap pen dix 1*).…”

Section: Radiocarbon Datingmentioning

confidence: 99%

Asynchronous development of two Late Glacial lake basins near the Drwęca ice-marginal valley (N Poland)

Gamrat

Błaszkiewicz²,

Andrzejewski

et al. 2017

View full text Add to dashboard Cite

IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP

Cited by 4,062 publications

References 120 publications

A decadally-resolved paleohurricane record archived in the late Holocene sediments of a Florida sinkhole

A decadally-resolved paleohurricane record archived in the late Holocene sediments of a Florida sinkhole

Grãos de pólen de angiospermas do Holoceno (7908±30 anos AP-atual) da Planície Costeira sul-catarinense, Brasil

Asynchronous development of two Late Glacial lake basins near the Drwęca ice-marginal valley (N Poland)

Contact Info

Product

Resources

About