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Understanding rapid climate change: clues from the sedimentary record

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Title: Understanding rapid climate change: clues from the sedimentary record


1
Understanding rapid climate change clues from
the sedimentary record
  • Thomas Stevens
  • tstevens_at_alumni.jesus.ox.ac.uk

2
Climate change
  • Sedimentary record evidence of changing climate
  • Sedimentology central role
  • Palaeoclimatology interdisciplinary, infancy,
    explosion of research since Shackleton and Opdyke
    1973 V28-238
  • Focus shifted to the study of sediments for
    climates sake

3
Unpleasant surprises?
  • 1980-90s increasing evidence for dramatic and
    abrupt shifts in climate
  • Abrupt climate change
  • when the climate system is forced to cross some
    threshold, triggering a transition to a new state
    at a rate determined by the climate system itself
    and faster than the cause (Alley et al., 2003).
  • An unpleasant surprise in store? Broecker (1987)
  • IPCC models not able to model rapid changes well
  • Focus shifts to sediments

4
Heinrich events
  • Abrupt collapse of NH ice sheets - cooling
  • Last hundreds of years, onset in years
  • 6 identified in late Quaternary more earlier?

Bond et al., 1992
  • Lithics in N Atlantic ocean cores ice bergs
  • Other evidence
  • 2.3x106 km3 freshwater
  • 7 kyr cyclicity
  • Cause internal or external?
  • Focused on N. Atlantic but do they propagate to
    other locations?

5
Dansgaard-Oeschger events
Greenland Ice Core Data
  • Rapid climate changes of period 1.470.5 ka
  • Identified strongly in glacials, weakly in
    Holocene
  • Identified from Greenland (5-8 C warming) ice
    core records
  • NH rapid warming (decades or less), slow
    cooling
  • SH slow warming, less intense precede? So
    called AIM events.
  • Causes solar (Bond et al. 2001)/ internal
    (THC/ice sheets/wind field/harmonic)

6
H and D-O events recent picture
  • Pervasive D-O events seen in pre-Late
    Quaternary records (loess, Antarctic ice
    650-800 ka)
  • Near global extent Asia, Africa, Americas,
    Antarctica
  • Many rapid proxy changes are seen as regional
    manifestations
  • Typified by the loess record in China (e.g.
    Porter and An, 1995 and more recently Guan et
    al., in press).
  • Some recent caveats

Porter and An, 1995, Nature
7
Chinese loess
  • Chinese loess wind blown silt
  • Quartz, micas, feldspars, massive
  • Up to 400m Chinese Loess Plateau
  • Miocene - Holocene
  • Chinese loess considered key monsoon archive
  • Terrestrial equivalent of ocean sediments

8
Caveats - 1
  • Synchronicity of events?
  • Changes linked across world
  • New evidence suggests this is problematic
  • Age models

Porter and An, 1995, Nature
Stevens et al., 2008, Geology
9
Caveats - 2
  • Lateral sedimentary facies differences
  • V. small changes used to infer abrupt shifts
    noise?

Porter and An, 1995, Nature
Stevens and Lu, in press, Sedimentology
10
Caveats - 3
  • Complex and site specific sedimentary processes
  • Independently calculated SRs
  • Many sites needed

Stevens and Lu in press, Sedimentology
11
Caveats - 4
  • D-O events restricted to the Greenland??
  • claims, however, of D-O presence in most remote
    locations cannot be distinguished from the
    hypothesis that many regions are just
    experiencing temporal variability in climate
    proxies with approximately similar frequency
    content Wunsch (Quaternary Research, 2006)

Greenland Ice Core Data
12
More uncertainties
  • Pre Quaternary evidence pervasive?
  • Carbonate beds should be evidence
  • Tucker in ISC 2006
  • Spectral analysis problematic?
  • Spurious cycles depositional complexities
  • Lu et al., 2004.
  • GCMs
  • Poor at simulating apparent distribution of rapid
    climate change

13
Evidence for H events in loess record?
  • Heinrich Events?
  • Some examples of match

14
Evidence for H events in loess record?
  • Heinrich Events?
  • Some examples of match
  • Some examples of no change

15
Evidence for H events in loess record?
  • Heinrich Events?
  • Some examples of match
  • Some examples of no change
  • Some examples of change and no H event (or close
    but not quite)

16
Evidence for H events in loess record?
  • Heinrich Events?
  • Some examples of match
  • Some examples of no change
  • Some examples of change and no H event (or close
    but not quite)
  • Complex interaction of monsoon with site
    specifics
  • No firm evidence?

17
Challenges in light of this
  • What is the geographic distribution?
  • What is the relative timing?
  • Terrestrial evidence?
  • Pre-Quaternary evidence?

18
New approach
  • Marrying sedimentology into multi-discipline
    palaeoclimatology
  • Palaeoclimatologists seldom sedimentologists
  • Sedimentary evidence of rapid sediment
    emplacement (gas escape structures, giant
    ripples, rip up clasts, abrupt grain-changes,
    micromorphological analyses etc)
  • Geochronology timing and duration
  • Relative timing and distribution elucidates the
    causes
  • CO2 driven and/or propagated?

P. Hoffman
19
Thanks for your attention
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