280159 VO+SE MA-ERD-W-1.1 Paleoceanography and Climate Change (PI) (2021W)
Prüfungsimmanente Lehrveranstaltung
Labels
VOR-ORT
An/Abmeldung
Hinweis: Ihr Anmeldezeitpunkt innerhalb der Frist hat keine Auswirkungen auf die Platzvergabe (kein "first come, first served").
- Anmeldung von Mi 08.09.2021 10:00 bis Mi 29.09.2021 23:59
- Anmeldung von Fr 01.10.2021 10:00 bis Mi 13.10.2021 23:59
- Abmeldung bis Mi 13.10.2021 23:59
Details
max. 20 Teilnehmer*innen
Sprache: Englisch
Lehrende
Termine (iCal) - nächster Termin ist mit N markiert
Montag 29.11.2021: 09.00-13.00; Ort: Übungssaal der Paläontologie 2A225 UZA II
Dienstag 30.11.2021: 09.00-13.00; Ort: Übungssaal der Paläontologie 2A225 UZA II
Mittwoch 01.12.2021: 09.00-13.00; Ort: Hörsaal 1 2A120 UZA II
Donnerstag 02.12.2021: 09.00-13.00 Ort: Mikroskopiepraktikum Geowissenschaften 2A205 2.OG UZA II
Freitag 3.12.2021: 09.00-13.00 Ort: Übungssaal der Paläontologie 2A225 UZA II
- Mittwoch 01.12. 09:00 - 12:45 Hörsaal 1 2A120 1.OG UZA II Geo-Zentrum
- Donnerstag 02.12. 09:00 - 12:45 Mikroskopiepraktikum Geowissenschaften 2A205 2.OG UZA II
Information
Ziele, Inhalte und Methode der Lehrveranstaltung
This course will explore the ocean-climate system from a geological perspective, with particular emphasis on the past 65 million years of Earth’s history. Students will learn about the ocean-climate connection today and will explore how physical, chemical, and biological aspects of ocean and climate leave characteristic imprints in marine sediments and what are the tools available to scientists to extract and read such clues. Students will also learn about specific past climatic regimes (e.g., greenhouse periods, rapid climatic perturbations, and transitions to cooler climates). The course will be organized as a combination of lectures and discussion of scientific, peer-reviewed papers.
Art der Leistungskontrolle und erlaubte Hilfsmittel
Final exam on Friday 3 December 2021.
Mindestanforderungen und Beurteilungsmaßstab
At least 50% of the points in the final exam have to be reached.rating:
87,5-100% = 1;
75-87,4% = 2;
62,5-74,9% = 3;
50-62,4% = 4
87,5-100% = 1;
75-87,4% = 2;
62,5-74,9% = 3;
50-62,4% = 4
Prüfungsstoff
Lecture PDFs and additional provided study material.
Literatur
Trujillo, A. P., & Thurman, H. V. (2020). Essentials of oceanography - Chapters 2 and 7. Upper Saddle River, N.J: Pearson Prentice Hall.Cronin, T. M., (2009). Paleoclimates : Understanding Climate Change Past and Present - Chapters 1 and 4. Columbia University Press. New York.Katz et al. (2010). Traditional and emerging geochemical proxies in foraminifera. Journal of Foraminiferal Research, 40(2), 165–192.The following papers will be discussed during class:
1) Tuesday: McInerney, F. A., and Wing, S. L. (2011). The Paleocene-Eocene Thermal maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future. Annual Review of Earth and Planetary Sciences, 39, 489–516.
2) Wednesday: Hutchison, D. K., et al. (2021). The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons. Climate of the Past, 17, 269–315.
3) Thursday: Berends, C. J., Köhler, P., Lourens, L. J., and van de Wal, R. S. W. (2021). On the cause of the mid-Pleistocene transition. Reviews of Geophysics, 59, e2020RG000727.
1) Tuesday: McInerney, F. A., and Wing, S. L. (2011). The Paleocene-Eocene Thermal maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future. Annual Review of Earth and Planetary Sciences, 39, 489–516.
2) Wednesday: Hutchison, D. K., et al. (2021). The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons. Climate of the Past, 17, 269–315.
3) Thursday: Berends, C. J., Köhler, P., Lourens, L. J., and van de Wal, R. S. W. (2021). On the cause of the mid-Pleistocene transition. Reviews of Geophysics, 59, e2020RG000727.
Zuordnung im Vorlesungsverzeichnis
Letzte Änderung: Do 31.10.2024 00:16