Age model of sediment core NBP99-03_10


Autoria(s): Etourneau, Johan; Collins, LG; Willmott, Verónica; Kim, Jung-Hyun; Barbara, Loïc; Leventer, Amy; Schouten, Stefan; Sinninghe Damsté, Jaap S; Bianchini, A; Klein, V; Crosta, Xavier; Massé, Guillaume
Cobertura

LATITUDE: -64.883330 * LONGITUDE: -64.200000 * MINIMUM DEPTH, sediment/rock: 0.105 m * MAXIMUM DEPTH, sediment/rock: 13.230 m

Data(s)

30/08/2013

Formato

text/tab-separated-values, 36 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.818908

doi:10.1594/PANGAEA.818908

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.818912

Etourneau, Johan; Collins, LG; Willmott, Verónica; Kim, Jung-Hyun; Barbara, Loïc; Leventer, Amy; Schouten, Stefan; Sinninghe Damsté, Jaap S; Bianchini, A; Klein, V; Crosta, Xavier; Massé, Guillaume (2013): Holocene climate variations in the western Antarctic Peninsula: evidence for sea ice extent predominantly controlled by changes in insolation and ENSO variability. Climate of the Past, 9(4), 1431-1446, doi:10.5194/cp-9-1431-2013

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #Age, comment; Calendar years; Climate Change: Learning from the past climate; DEPTH, sediment/rock; Nathaniel B. Palmer; NBP99-03; NBP99-03_10; Palmer Deep Basin; Past4Future; PC; Piston corer; Sedimentation rate per year
Tipo

Dataset