619 resultados para Lind, Tuula


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We present an unprecedented multicentennial sediment record from the foot of Vesterisbanken Seamount, central Greenland Sea, covering the past 22.3 thousand years (ka). Based on planktic foraminiferal total abundances, species assemblages, and stable oxygen and carbon isotopes, the palaeoenvironments in this region of modern deepwater renewal were reconstructed. Results show that during the Last Glacial Maximum the area was affected by harsh polar conditions with only episodic improvements during warm summer seasons. Since 18?ka extreme freshwater discharges from nearby sources occurred, influencing the surface water environment. The last major freshwater event took place during the Younger Dryas. The onset of the Holocene was characterized by an improvement of environmental conditions suggesting warming and increasing ventilation of the upper water layers. The early Holocene saw a stronger Atlantic waters advection to the area, which began around 10.5 and ended quite rapidly at 5.5?ka, followed by the onset of Neoglacial cooling. Surface water ventilation reached a maximum in the middle Holocene. Around 3?ka the surface water stratification increased leading to subsequent amplification of the warming induced the North Atlantic Oscillation at 2?ka.

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Mode of access: Internet.

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V. 1-2 published by Th. Lind.

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[1st ser.] Faustina Bordoni. Catarina Gabrielli. Sophie Arnould. Elizabeth Billington and her contemporaries. Angelica Catalani. Giuditta Pasa. Henrietta Sontag.--2d ser. Maria Felicia Malibran. Wilhelmina Schröder-Devrient. Giulia Grisi. Pauline Viardot. Fanny Persiani. Marietta Alboni. Jenny Lind. Sophie Cruvelli. Theresa Titiens.

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Binder's title.

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Mode of access: Internet.