| d.fossileShapes | R Documentation |
The abundance of cocolith shells can be used to infer environmental conditions in epochs corresponding to earlier epochs. This data set contains the core location, the relative abundance of Gephyrocapsa morphotypes and the sea surface temperatures from all deep see cores used in this study.
data("d.fossileShapes")
data("d.fossileSamples")
d.fossilShapes:
A data frame with 5864 observations on the following 15
variables:
Identification and location of the sample:
SampleIdentification number of the sample
SnameIdentification code
Magnification(technical)
Shape features and recommended transformations:
Anglebridge angle
Length, Widthlengtha and width of the shell
CLength, CWidthlength and width of the 'central area'
Cratioratio between width and length of the central area
sAnglesqrt of Angle
lLengthlog10(Length)
rWidth, rCLength, rCWidthrelative measures,
percentage of Length
CratioCWidth/Clength
ShapeClassshape class as defined in the cited paper,
classes ar
CM < CC < CT < CO < CE < CL
d.fossilSamples:
A data frame with 108 observations on the following 32
variables:
Identification and location:
SampleIdentification number of the sample (as above)
SnameIdentification code
Latitude, LongitudeCoordinates of the location
RegionOcean: Pacific, Atlantic, Indian.Ocean
SDepthsample depth below soil surface [cm]
WDepthWater depth [m]
Nnumber of specimen measured
Shape features as above, averaged.
(This is the reason for introducing transformed variables above:
The transformed values are averaged.)
CM, CC, CT, CO, CE, CLpercentages of shape classes in the sample
Environment:
SSTSea Surface Temperature, mean, [deg C]
SST.Spring, SST.Summer, SST.Fall,
SST.Winter... in each season
Chlorophyll, lChlorophyllChlorophyll content
[microgram/L] and log10 of it
SalinitySalinity of the sea water
The paradigm of research associated with this dataset is the following: Datasets of this kind are used to establish the relationship between the shell shapes of cocoliths (species Gephyrocapsa) from the most recent sediment layer with actual environmental conditions. This relationship is then used to infer environmental conditions of earlier epochs from the shell shapes from the corresponding layers.
The analysis presented in the paper cited below consisted of first introducing classes of shells based on the shapes and then use the relative abundance of the classes to predict the environmental conditions.
J\"org Bollmann, Jorijntje Henderiks and Bernhard Brabec (2002). Global calibration of Gephyrocapsa coccolith abundance in Holocene sediments for paleotemperature assessment. Paleoceanography, 17(3), 1035
J\"org Bollmann (1997). Morphology and biogeography of Gephyrocapsa coccoliths in Holocene sediments. Marine Micropaleontology, 29, 319-350
data(d.fossileShapes)
names(d.fossileShapes)
data(d.fossileSamples)
plyx(sqrt(Angle) ~ SST, data=d.fossileSamples)
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