Title: Understanding rapid climate change: clues from the sedimentary record
1Understanding rapid climate change clues from
the sedimentary record
- Thomas Stevens
- tstevens_at_alumni.jesus.ox.ac.uk
2Climate 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
3Unpleasant 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
4Heinrich 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?
5Dansgaard-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)
6H 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
7Chinese 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
8Caveats - 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
9Caveats - 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
10Caveats - 3
- Complex and site specific sedimentary processes
- Independently calculated SRs
- Many sites needed
Stevens and Lu in press, Sedimentology
11Caveats - 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
12More 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
13Evidence for H events in loess record?
- Heinrich Events?
- Some examples of match
14Evidence for H events in loess record?
- Heinrich Events?
- Some examples of match
- Some examples of no change
15Evidence 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)
16Evidence 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?
17Challenges in light of this
- What is the geographic distribution?
- What is the relative timing?
- Terrestrial evidence?
- Pre-Quaternary evidence?
18New 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
19Thanks for your attention