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Additional observations of Spiniferites alaskensis from topotype material ArchiMer
Marret, Fabienne; Mertens, Kenneth.
Here we present new observations of Spiniferites alaskensis, a relatively rare species described from the Eemian of the Gulf of Alaska. We show that the species shows a gonyaulacacean tabulation: Po, 4´, 6´´, 6c,? s, 6´´´, 1p, 1´´´´. The surface is finely granulate to scabrate. The species bears characteristic processes: these are exclusively gonal, membranous, perforated and end distally in platforms with stumpy ends. We provide more detail as how this species compares to closely related species belonging to the genus Spiniferites.
Tipo: Text Palavras-chave: Gulf of Alaska; Chorate; Spiniferites; Processes; Eemian; ODP.
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00471/58307/60848.pdf
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Direct terrestrial-marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe ArchiMer
Sier, Mark J.; Roebroeks, Wil; Bakels, Corrie C.; Dekkers, Mark J.; Bruehl, Enrico; De Loecker, Dimitri; Gaudzinski-windheuser, Sabine; Hesse, Norbert; Jagich, Adam; Kindler, Lutz; Kuijper, Wim J.; Laurat, Thomas; Muecher, Herman J.; Penkman, Kirsty E. H.; Richter, Daniel; Van Hinsbergen, Douwe J. J..
An interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 +/- 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e 'peak' in the marine record and the start of the last interglacial in this region.
Tipo: Text Palavras-chave: Blake Event; Eemian; Last interglacial; MIS 5e; Palaeomagnetism.
Ano: 2011 URL: https://archimer.ifremer.fr/doc/00228/33891/32225.pdf
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Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130,000 years based on diatoms and with comparison to foraminiferal records ArchiMer
Hoff, Ulrike; Rasmussen, Tine L.; Meyer, Hanno; Koc, Nalan; Hansen, Jesper.
Fossil marine diatom assemblages in a sediment core from the central northern Faroe slope in the Norwegian Sea were used to reconstruct palaeoceanographic changes in the surface water mixed layer from the last similar to 130,000 years (Marine Isotope Stage (MIS) 6/5 transition to MIS 1 (including the Eemian and Holocene interglacials) and to compare the results with previously published results on planktic foraminifera representing the subsurface conditions of the thermocline. Diatom floras from MIS 5 of the Nordic seas have rarely been studied in detail before and never the entire period from pre-Eemian to present. The composition of diatom species together with maxima in absolute abundance of diatoms, indicate two periods of warmer sea surface...
Tipo: Text Palavras-chave: Atlantic water; Marine isotope stages (MIS); Eemian; Holocene; Faroe Islands; Nordic seas.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00504/61586/65893.pdf
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