Lebreiro, Susana Martin; Moreno, J C; McCave, I Nick; Weaver, Philip PE (1996): Mineralogy and age determination of sediment core D11957P [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.734083, Supplement to: Lebreiro, SM et al. (1996): Evidence for Heinrich layers off Portugal (Tore Seamount: 39°N, 12°W). Marine Geology, 131(1-2), 47-56, https://doi.org/10.1016/0025-3227(95)00142-5
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
The Tore Seamount is a circular, volcano-like feature 100 km in diameter with its summit at 2200 m water depth and a small, 5000 m deep basin in its interior. It is situated approximately 300 km west of Lisbon and is surrounded by deep abyssal plains. This site with a standard pelagic stratigraphy is the southernmost point where the so-called Heinrich events have so far been recorded.
A succession of alternating interglacial/glacial periods reveals a stratigraphic record back to the beginning of isotopic stage 7 (225 kyr). Climatic changes are identifiable by coherent variations in colour, carbonate content and distribution of ice-rafted detritus in the carbonate-free fraction. Inputs of ice-rafted quartz are well defined. Characteristics in common with other sites showing Heinrich layers include a high terrigenous to biogenic ratio, a dramatic decrease in the accumulation rate of foraminifera shells, an increase in dolomite abundance and the occurrence of polar foraminiferal species indicating southwards penetration of cold waters which lead us to consider a wider southeastern extent of the North Atlantic ice-rafted detritus belt than hitherto. If the presently accepted position of the Polar Front is maintained, icebergs must have been swept southwards from the southern boundary of the pack ice in a current merging into the ancestral Canary Current, bringing ice-rafted material to the Tore Seamount. The coincidence of reddish-feldspar, probably derived from the northern Appalachian Triassic red facies, with the transparent quartz suggests at least a partial Labrador source for all the Heinrich layers here, including HL 3. In comparison to other sites in the entire North Atlantic, two exceptions stand out: the absence of HL 5 and the low detritus to biogenics ratio for HL 3. The simultaneous occurrence of these two types of ice-rafted minerals is a new piece in the puzzle of the origin of Heinrich layers.
Coverage:
Latitude: 39.050000 * Longitude: -12.583333
Date/Time Start: 1989-11-15T00:00:00 * Date/Time End: 1989-11-15T00:00:00
Event(s):
D11957P * Latitude: 39.050000 * Longitude: -12.583333 * Date/Time: 1989-11-15T00:00:00 * Elevation: -3585.0 m * Recovery: 6.35 m * Campaign: D187 * Basis: Discovery (1962) * Method/Device: Piston corer (PC)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
Download Data
Datasets listed in this publication series
- Lebreiro, SM; Moreno, JC; McCave, IN et al. (1996): (Fig. 3) Age model of sediment core D11957P. https://doi.org/10.1594/PANGAEA.53372
- Lebreiro, SM; Moreno, JC; McCave, IN et al. (1996): (Table 2) Comparison between dolomite, calcite and quartz for Heinrich layers and the interlayered intervals of sediment core D11957P. https://doi.org/10.1594/PANGAEA.734082