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Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 1
Dr. Ankit → Landscape Geoscience & Fire (3rd Floor, 3.177)
Climate-Bio-Geo-Chemical feedbacks during the extreme environmental conditions on planet Earth
Molecular tracers
Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 2
• Pliocene environmental changes in the Levantine Corridor (Near East)
• Changes in Black Carbon composition and sequestration: an assessment based on lake sediments in Higher
Himalayas
• Change, Resilience, Transitions and Sustainability in the Indian subcontinent during the late Holocene:
Investigating environmental variability and human disturbances with biogeochemical fingerprinting of
lacustrine records
• Climate-Biogeochemical feedbacks during the extreme environmental conditions in the history of planet
Earth: A picture from PETM and end-Permian mass extinction
Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 3
The core hypothesis is that insolation maxima in the tropics is
the main controlling mechanism behind the sustainability of
ephemeral palustrine systems in mid-latitude regions during
the Plio-Pleistocene, which in turn served as windows of
opportunity that greened the path and permitted large-scale
faunal dispersal (including humans)
Pliocene environmental changes in the Levantine Corridor (Near East)
Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 4
Changes in Black Carbon (BC) composition and sequestration
Deposition of Organic contaminants in the high-altitude lakes
Source apportionment using molecular fossils and their isotopic composition
Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 5
Anthropogenic forcing of each region?
Regional differences in sensitivity of different components of the ecosystem to climate forcings?
Change, Resilience, Transitions and Sustainability in the Indian subcontinent during
the late Holocene: Investigating climate variability and human disturbances with
biogeochemical fingerprinting of lacustrine records
Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 6
2
3
1
2
1
251-255 Ma
Climate-Biogeochemistry feedbacks during the extreme environmental conditions in the history of planet Earth
A picture from PETM and end-Permian mass extinction
Causal Mechanisms (Flooding, Fire and etc.)
Relative greenhouse gas concentrations
Recovery of different environments

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Masters Seminar.pptx

  • 1. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 1 Dr. Ankit → Landscape Geoscience & Fire (3rd Floor, 3.177) Climate-Bio-Geo-Chemical feedbacks during the extreme environmental conditions on planet Earth Molecular tracers
  • 2. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 2 • Pliocene environmental changes in the Levantine Corridor (Near East) • Changes in Black Carbon composition and sequestration: an assessment based on lake sediments in Higher Himalayas • Change, Resilience, Transitions and Sustainability in the Indian subcontinent during the late Holocene: Investigating environmental variability and human disturbances with biogeochemical fingerprinting of lacustrine records • Climate-Biogeochemical feedbacks during the extreme environmental conditions in the history of planet Earth: A picture from PETM and end-Permian mass extinction
  • 3. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 3 The core hypothesis is that insolation maxima in the tropics is the main controlling mechanism behind the sustainability of ephemeral palustrine systems in mid-latitude regions during the Plio-Pleistocene, which in turn served as windows of opportunity that greened the path and permitted large-scale faunal dispersal (including humans) Pliocene environmental changes in the Levantine Corridor (Near East)
  • 4. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 4 Changes in Black Carbon (BC) composition and sequestration Deposition of Organic contaminants in the high-altitude lakes Source apportionment using molecular fossils and their isotopic composition
  • 5. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 5 Anthropogenic forcing of each region? Regional differences in sensitivity of different components of the ecosystem to climate forcings? Change, Resilience, Transitions and Sustainability in the Indian subcontinent during the late Holocene: Investigating climate variability and human disturbances with biogeochemical fingerprinting of lacustrine records
  • 6. Sauer et al.: nFK → Regenerationspotential von Wäldern der mongolischen Waldsteppe 6 2 3 1 2 1 251-255 Ma Climate-Biogeochemistry feedbacks during the extreme environmental conditions in the history of planet Earth A picture from PETM and end-Permian mass extinction Causal Mechanisms (Flooding, Fire and etc.) Relative greenhouse gas concentrations Recovery of different environments

Editor's Notes

  1. A very Good afternoon to everyone. I thank Professor Sauer for the nice introduction. As she have already stated that I am an akademischer rat in Department of Physical Geography and I specialize in the field of Biogeochemistry including biochemistry, organic chemistry, isotope chemistry, environmental chemistry and analystical chemistry. My research focuses on understanding the climate-bio-geo-chemical feedbacks during the extreme environmental conditions on our planet. To understand all these attrbutes, I use a multi-archive approach with an integrated multi-proxy investigation. I mainly deal with molecular fossils or tracers archived in different environmental archives like different aquatic environments, geological rock samples, modern day particulate material and etc. So with this I will present results from one of my investigations focusing on understanding the climate-human and environmental relations in the Himalayan ecotone.