(Table 3) Oxygen and carbon isotopes of Planulina wuellerstorfi and/or Cibicidoides kullenbergi from DSDP Hole 72-517


Autoria(s): Hodell, David A; Kennett, James P; Leonard, Kathleen A
Cobertura

LATITUDE: -30.946800 * LONGITUDE: -38.041200 * DATE/TIME START: 1980-03-30T00:00:00 * DATE/TIME END: 1980-03-30T00:00:00 * MINIMUM DEPTH, sediment/rock: 36.5 m * MAXIMUM DEPTH, sediment/rock: 50.7 m

Data(s)

30/05/1983

Formato

text/tab-separated-values, 45 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.814007

doi:10.1594/PANGAEA.814007

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.814013

Hodell, David A; Kennett, James P; Leonard, Kathleen A (1983): Climatically induced changes in vertical water mass structure of the Vema Channel during the Pliocene: evidence from Deep Sea Drilling Project Holes 516A, 517, and 518. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 907-919, doi:10.2973/dsdp.proc.72.146.1983

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #72-517; AGE; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg72; Mass spectrometer VG Micromass 602; ODP sample designation; Planulina wuellerstorfi, d13C; Planulina wuellerstorfi, d18O; Sample code/label; South Atlantic/FLANK
Tipo

Dataset