Data Description

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Pflaumann, U et al. (1996): Distribution of planktic foraminifera in surface sediments of the Atlantic Ocean. doi:10.1594/PANGAEA.51621,
Supplement to: Pflaumann, Uwe; Duprat, Josette; Pujol, Claude; Labeyrie, Laurent D (1996): SIMMAX: A modern analog technique to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments. Paleoceanography, 11(1), 15-36, doi:10.1029/95PA01743
We present a data set of 738 planktonic foraminiferal species counts from sediment surface samples of the eastern North Atlantic and the South Atlantic between 87°N and 40°S, 35°E and 60°W including published Climate: Long-Range Investigation, Mapping, and Prediction (CLIMAP) data. These species counts are linked to Levitus's [1982] modern water temperature data for the four caloric seasons, four depth ranges (0, 30, 50, and 75 m), and the combined means of those depth ranges. The relation between planktonic foraminiferal assemblages and sea surface temperature (SST) data is estimated using the newly developed SIMMAX technique, which is an acronym for a modern analog technique (MAT) with a similarity index, based on (1) the scalar product of the normalized faunal percentages and (2) a weighting procedure of the modern analog's SSTs according to the inverse geographical distances of the most similar samples. Compared to the classical CLIMAP transfer technique and conventional MAT techniques, SIMMAX provides a more confident reconstruction of paleo-SSTs (correlation coefficient is 0.994 for the caloric winter and 0.993 for caloric summer). The standard deviation of the residuals is 0.90°C for caloric winter and 0.96°C for caloric summer at 0-m water depth. The SST estimates reach optimum stability (standard deviation of the residuals is 0.88°C) at the average 0- to 75-m water depth. Our extensive database provides SST estimates over a range of -1.4 to 27.2°C for caloric winter and 0.4 to 28.6°C for caloric summer, allowing SST estimates which are especially valuable for the high-latitude Atlantic during glacial times.
Further details:
Pflaumann, Uwe (1996): Source code of SIMMAX28 software for paleotemperature calculations from planktonic foraminifera assemblages. doi:10.1594/PANGAEA.59332
Glacial Atlantic Ocean Mapping (GLAMAP2000) *
Median Latitude: 27.318100 * Median Longitude: -15.686497 * South-bound Latitude: -39.820000 * West-bound Longitude: -69.500000 * North-bound Latitude: 85.390000 * East-bound Longitude: 30.850000
Date/Time Start: 1953-07-30T00:00:00 * Date/Time End: 1992-07-21T00:00:00
Minimum DEPTH, sediment/rock: 0.0 m * Maximum DEPTH, sediment/rock: 0.0 m
A152-84 * * Latitude: 44.349800 * Longitude: -30.267000 * Date/Time: 1960-01-01T00:00:00 * Elevation: -2750.0 m * Campaign: A150/180 * * Device: Piston corer (PC) * * Comment: Project/Cruise uncertain
A153-154 * * Latitude: 28.000000 * Longitude: -38.783000 * Date/Time: 1960-01-01T00:00:00 * Elevation: -4020.0 m * Location: Atlantic * * Campaign: A150/180 * * Device: Piston corer (PC) * * Comment: Project/Cruise uncertain
A157-3 * * Latitude: 50.933200 * Longitude: -41.750000 * Date/Time: 1960-01-01T00:00:00 * Elevation: -4025.0 m * Campaign: A150/180 * * Device: Piston corer (PC) * * Comment: Project/Cruise uncertain
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Event label *Event
2Date/Time of event *Date/Time
3LATITUDE *Latitude
4LONGITUDE *Longitude
5Elevation of event *Elevationm
6DEPTH, sediment/rock *Depthm
7Globigerinella aequilateralis *G. aequilateralis%Pflaumann, Uwe *Counting >150 µm fraction *
8Globigerina bulloides *G. bulloides%Pflaumann, Uwe *Counting >150 µm fraction *
9Globigerinella calida *G. calida%Pflaumann, Uwe *Counting >150 µm fraction *
10Globigerinoides conglobatus *G. conglobatus%Pflaumann, Uwe *Counting >150 µm fraction *
11Globorotalia crassaformis *G. crassaformis%Pflaumann, Uwe *Counting >150 µm fraction *
12Sphaeroidinella dehiscens *S. dehiscens%Pflaumann, Uwe *Counting >150 µm fraction *
13Globigerina digitata *G. digitata%Pflaumann, Uwe *Counting >150 µm fraction *
14Globoquadrina dutertrei *G. dutertrei%Pflaumann, Uwe *Counting >150 µm fraction *
15Globigerina falconensis *G. falconensis%Pflaumann, Uwe *Counting >150 µm fraction *
16Globigerinita glutinata *G. glutinata%Pflaumann, Uwe *Counting >150 µm fraction *
17Globorotalia hirsuta *G. hirsuta%Pflaumann, Uwe *Counting >150 µm fraction *
18Globorotalia inflata *G. inflata%Pflaumann, Uwe *Counting >150 µm fraction *
19Pulleniatina obliquiloculata *P. obliquiloculata%Pflaumann, Uwe *Counting >150 µm fraction *
20Neogloboquadrina pachyderma sinistral *N. pachyderma s%Pflaumann, Uwe *Counting >150 µm fraction *
21Neogloboquadrina pachyderma dextral and dutertrei integrade *P/D int%Pflaumann, Uwe *Counting >150 µm fraction *
22Globigerina quinqueloba *G. quinqueloba%Pflaumann, Uwe *Counting >150 µm fraction *
23Globigerinoides ruber pink *G. ruber p%Pflaumann, Uwe *Counting >150 µm fraction *
24Globigerinoides ruber white *G. ruber w%Pflaumann, Uwe *Counting >150 µm fraction *
25Globoturborotalita rubescens *G. rubescens%Pflaumann, Uwe *Counting >150 µm fraction *
26Globigerinoides trilobus trilobus *G. trilobus tril%Pflaumann, Uwe *Counting >150 µm fraction *
27Globigerinoides trilobus sacculifer *G. trilobus sac%Pflaumann, Uwe *Counting >150 µm fraction *
28Globorotalia cultrata *G. cultrata%Pflaumann, Uwe *Counting >150 µm fraction *including G. tumida
29Globorotalia scitula *G. scitula%Pflaumann, Uwe *Counting >150 µm fraction *
30Globigerinoides tenellus *G. tenellus%Pflaumann, Uwe *Counting >150 µm fraction *
31Globorotalia truncatulinoides sinistral *G. truncatulinoides s%Pflaumann, Uwe *Counting >150 µm fraction *
32Orbulina universa *O. universa%Pflaumann, Uwe *Counting >150 µm fraction *
33Foraminifera, planktic *Foram plankt#Pflaumann, Uwe *Counting >150 µm fraction *
34Sample code/label *Sample code/labelPflaumann, Uwe *Event label as given by the PI
35Comment *CommentPflaumann, Uwe *
21402 data points

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