The 41 kyr world: Milankovitch's other unsolved mystery

By M. Raymo, K. Nisancioglu. 2003

352 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/731a8a8c6bdf9bdac026428b68e4ddf531e182aa

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Anthropology

1. Simon Brewer
2. B. Davis
3. A. Broccoli
4. Ralf-Dietrich Kahlke

In Atmospheric Science

1. A. Hall
2. Michael Schulz
3. Simon Brewer
4. B. Davis
5. A. Clement
6. A. Broccoli
7. A. Ridgwell
8. M. Maslin

In Ecology

1. A. Hall
2. A. Clement
3. A. Broccoli
4. A. Ridgwell
5. M. Maslin
6. Ralf-Dietrich Kahlke
7. Stefan Rahmstorf

Citations in the corpus

• The importance of precessional signals in the tropical climate (2004, background): “1999), and there is an active debate as to the role of obliquity in late Quaternary climate change (Paillard 2001; Raymo and Nisancioglu 2003).”
• Regional climate shifts caused by gradual global cooling in the Pliocene epoch (2004, neutral): “Thus, variations in solar heating due to changes in the Earth's angle of tilt, or obliquity, must be an important driving force of glacial cycles before the Late Pleistocene perio”
• The origin of Eurasian Mammoth Faunas (Mammuthus–Coelodonta Faunal Complex) (2014, background): “Following a 41 ka periodicity in global temperature and climate evolution lastingmillions of years, and a subsequent period of more or less irregular variations between 1.2 and 0.9 Ma BP, the Middle and Late Pleistocene was governed by a clear 100 ka periodicity (Raymo and Nisancioglu, 2003, Fig.”
• Mid-Pleistocene revolution and the ‘eccentricity myth’ (2005, background): “Our aim here is to clarify the often confused role of eccentricity and review current theories of the MPR.”
• Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion (2007, background): “…whereas cool summers during periods of low obliquity would favor ice sheet growth, and (2) that high obliquity corresponding to low summer insolation gradient between low and high latitudes would decrease poleward moisture transport and reduce ice-sheet buildup (Raymo and Nisancioglu, 2003).”
• Orbital forcing and role of the latitudinal insolation/temperature gradient (2009, background): “Alternatively, Raymo and Nisancioglu (2003) have proposed that obliquity is important because of its influence on the summer LIG (Fig.”