Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Huang, Enqing; Mulitza, Stefan; Paul, André; Groeneveld, Jeroen; Steinke, Stephan; Schulz, Michael (2012): (Table 3) Planulina ariminensis δ¹⁸O and Mg/Ca, the predicted d18O of calcite and the calcification temperature of core top samples, as well as temperature, salinity, Delta[CO3**2-]calcite of bottom waters [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.802561, In supplement to: Huang, E et al. (2012): Response of eastern tropical Atlantic central waters to Atlantic meridional overturning circulation changes during the Last Glacial Maximum and Heinrich Stadial 1. Paleoceanography, 27, https://doi.org/10.1029/2012PA002294

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Coverage:
Median Latitude: 8.913929 * Median Longitude: -14.922833 * South-bound Latitude: 8.875500 * West-bound Longitude: -14.961000 * North-bound Latitude: 8.948000 * East-bound Longitude: -14.889333
Date/Time Start: 2005-06-26T10:26:00 * Date/Time End: 2005-06-26T23:12:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 2.000 m
Event(s):
GeoB9532-1 (317) * Latitude: 8.948000 * Longitude: -14.889333 * Date/Time: 2005-06-26T10:26:00 * Elevation: -301.0 m * Campaign: M65/1 * Basis: Meteor (1986) * Method/Device: MultiCorer (MUC) * Comment: 17-23 cm
GeoB9532-2 (317) * Latitude: 8.945333 * Longitude: -14.892000 * Date/Time: 2005-06-26T11:04:00 * Elevation: -317.0 m * Recovery: 3.16 m * Campaign: M65/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: geology, 316 cm
GeoB9533-2 (318) * Latitude: 8.926167 * Longitude: -14.910333 * Date/Time: 2005-06-26T13:57:00 * Elevation: -384.0 m * Recovery: 5.6 m * Campaign: M65/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: geology, 560 cm
Comment:
Delta d18O (Predicted - Measurement) is the difference between the predicted d18O of calcite and the P. ariminensis d18O.
The calcification temperature is calculated after equation (5).
Delta T is the difference between the calcification temperature and the bottom water temperature.
* Mean values of CTD stations GeoB9532-4, 9533-4, 9534-1, 9535-1.
# Data from the WOA2009 [Antonov et al., 2010; Locarnini et al., 2010].
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Latitude of eventLatitude
2Longitude of eventLongitude
3Elevation of eventElevationm
4Event labelEvent
5DEPTH, sediment/rockDepth sedmGeocode
6Depth, top/minDepth topmHuang, Enqing
7Depth, bottom/maxDepth botmHuang, Enqing
8Planulina ariminensis, Magnesium/Calcium ratioP. ariminensis Mg/Cammol/molHuang, EnqingICP-OES, Perkin-Elmer, Optima 3300RL
9Planulina ariminensis, δ18OP. ariminensis δ18O‰ PDBHuang, EnqingMass spectrometer Finnigan MAT 252
10Temperature, waterTemp°CHuang, Enqing
11SalinitySalHuang, Enqing
12Carbonate ion[CO3]2-µmol/kgHuang, EnqingCalculated by CO2sys_xls_program (Lewis and Wallace, 2006)
13δ18O, calciteδ18O cal‰ PDBHuang, Enqingpredicted
14Δδ18OΔδ18OHuang, EnqingCalculatedpredicted-measurement
15Temperature, waterTemp°CHuang, EnqingCalculatedcalcification
16Temperature, calculatedT cal°CHuang, EnqingCalculated
Size:
150 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML