Dataset - B2FIND

Isothermal Remanent Magnetization (IRM) acquisition curves for petrologically...

IRM acquisition curves (and their derivatives) resolve the cumulative coercivity distribution (and spectrum) of a magnetic mineral assemblage. Here we present data of larger,...

Rock magnetic properties of petrologically representative IRD particles in se...

In order to determine the bulk magnetic impact of all 22 classified IRD lithologies, the specific petromagnetic properties of each were investigated in detail. In order to...

Principal Component Analysis (PCA) of IRD content in Heinrich Event layers (H...

The data matrix of 192 classified IRD count data from H1-H5a and I1-I5 (excluding I6 because of too low IRD counts) by 22 IRD lithologies...

IRD composition and accumulation rates of Heinrich Event layers (H1-H5a) and ...

The cumulative classified count record (in percentages) over ~2 cm resolution of each petrologically identified IRD lithologies within the stratigraphic units of Heinrich Layers...

Magnetic workbook of Knapps Narrows sediment core from the Eastern Shore of M...

This dataset has no description

Updated ages for the McMurdo erratics and basis for age changes

LAD: last appearance datum, FAD: first appearance datum, LO: Last occurrence, LCO: Last common occurrence, FO: First occurrenceAntarctica New Zealand Sir Robin Irvine PhD...

Dinoflagellate cyst counts from IODP Hole 318-U1356A

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(Figure 10) Occurrence of coccoliths in two carbonate cycles at DSDP Hole 71-511

P = present, - = not present.

(Appendix 2a) Foraminiferal analyses of research borehole Sonder Vium

X = present,. - = absent.

(Appendix 2) Relative abundance of palynomorphs in ODP Hole 76-534A

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Fig 14. Pollen profile from sediment core Schmiecher See

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(Tab. 7) Occurence of microfossils in Late Jurassic sediments of DSDP Hole 50...

R = rare (1-5 specimens), C = common (6-20 specimens), A = abundante (significant occurence). Samples 50-416A-7-1,120-125, 50-416A-10-2,111-113, 50-416A-11-4,16-18,...