Global Element Cycles: Contemporary to Paleoenvironments
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Transcript of Global Element Cycles: Contemporary to Paleoenvironments
Global Element Cycles:Contemporary to Paleoenvironments
Richard Zeebe
Jane Schoonmaker
Telu Li
FredMackenzie
ChrisMeasures
TonyClarke
Brian Glazer
Barry Huebert
Kathleen Ruttenberg
EricDeCarlo
DavidHo
Global Element Cycles:Contemporary to Paleoenvironments
Will not review all research projects/PIs Examples
Big questions
(1) What is the human impact on global elemental cycles?
(2) How will ocean acidification affect carbonate production and dissolution?
(3) How can paleoclimatology help to predict climate changes?
(4) What are the roles of sediment geochemistry and seafloor-ocean exchange in sinks/sources of global elemental cycles?
(5) What do transient tracers tell us about changes in ocean circulation?
It will change the way we interpret the oceanic record
New 10-year program will provide - A coordinated Trace-Element and Isotope (TEI) survey of the oceans- Input for global C and climate models - A framework of chemical proxies for paleoceanography
GEOTRACES is starting and is already funded by NSF.
UH needs observational oceanographers to be able to take advantage of the funding associated with these programs.
Chris Measures(Steering Committee)
Global Element Cycles Expeditionary Programs (WOCE, CLIVAR, …)
Guiding mission
To identify processes and quantify fluxes that control the distributions of key trace elements and isotopes in the ocean, and to establish the sensitivity of these distributions to changing environmental conditions
AustraliaCanada (white)ChinaJapanKorea/JapanNew ZealandTaiwanU.S.
Tahiti EasterIsland
Hawaii
Global Element Cycles GEOTRACES
Science Plan:www.geotraces.org
Global Element Cycles Transient Tracers
What do transient tracers tell us about changes in ocean circulation?
DavidHo
Jenkins et al.
Global Element Cycles Geochemistry
Telu Li
Relationship among the nitrate deficit by denitrification (dN”), nitrite (NO2-), and oxygen (O2) concentrations in the eastern Pacific Ocean.
Data analyses: understand global biogeochemical cycles
Global Element Cycles Geochemistry
Lake Biwa: Largest fresh water lake in Japan
BIWA OCEAN
understand similarities/differences between fresh water systems and ocean.
Global Element Cycles Ocean acidification
FredMackenzie
Changes in carbonate chemistry and carbonate saturation state of the surface ocean from 1700 to 2300 based on modelcalculations.
Support: NOAA Coastal Ocean (Kathleen, Eric)
Global Element Cycles CaCO 3 production and dissolution
Cross over
Dissolution
Production
Coral reef environments of the Hawaiian Islands
Global Element Cycles Ocean acidification
Richard Zeebe
Support:- Department of Energy- NSF
Simulated changes in CaCO3 saturation state using aglobal biogeochemical ocean model:
YEAR 1810 YEAR 2100
PaleoclimatologyWhy bother about the past?
Two very recent examples:
Paleoclimatology
Sedimentary Records of Climate Change – Hawaii, Pacific, and
Beyond
Objectives• Understanding interactions between climate, hydrology,
ecosystems, human impacts• Revealing paleoclimate forcings and predicting future system
behavior
Jane Schoonmaker
B. Popp, A. Timmermann, (K. Pahnke)
Jane Schoonmaker
G&G
• Integrating data with climate models• Informing Hawaii state planning
Ordy Pond, OahuPaleoaridity Record
Paleoclimatology
Precipitation Anomaly
+ -20ºN Latitude of Hawaii
PaleoclimatologyOrdy Pond, OahuPaleoaridity Record
13C ( permil, VPDB )
-32 -30 -28 -26 -24 -22
Age
( ca
.kyr
BP
)
0
2
4
6
8
10
( A )
% C4 Plants Abundance
20 40 60 80 100
Age
( ca
.kyr
BP
)
0
2
4
6
8
10
( B )
Post-Human Contact
Increasing aridity
% C4 Plantsn-alkane 13C20 60 100-32 -28 -24
Post-HumanContact
2
6
8
10
4
+
-
Ag
e (k
yr B
P)
Paleoclimatology
What’s Next?
• Add additional proxies to the list: hydrogen isotopes, pollen, diatoms…
• Another try at acquiring Ordy• Other locations: Ka’au Crater, Lk. Kauhakō, Lk. Waiau, Niihau,
Easter Island…..
Support: NOAA Sea Grant
Petroleum Research Fund
Paleoclimatology PETM
Richard Zeebe
PETM
The Paleocene-Eocene Thermal Maximum (PETM), a future analog?
Support: NSF (Multi-Institutional
Project, $2.3M).
Ocean acidification
Ocean acidification
Links past, present, and future
Projects
• Carbon fluxes• Early detection of acidification effects
Support:- Department of Energy- NSF
Needs (to be continued by Frank)
• Chris: Hire expeditionary oceanographers (GEOTRACES)
• Post-doc support (admin, office space, new fellowships)
• Faculty hire/retention (cost of living/housing)
Global Element Cycles GEOTRACES
One of the three global planning workshops was held in Hawaiibringing funding and recognition to the state.
An international training workshop is being planned for 2009.
Paleoclimatology
FredMackenzie
Simulated changes in ocean chemistry over the Phanerozoic (500 Ma).
Support: - NSF- NOAA Sea Grant