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David C Lund
University Of Connecticut
$3,573,228
Attributed
$3,573,228
Total exposure
12
Grants
12
Lead (contact PI)
Attributed= this PI's even-split share of every grant they're on (the fair, additive number). Exposure = full size of all those grants. They are the sole PI on all grants (the two match).
Funding over time
peak $840.1K · FY2010–24$1M$750K$500K$250K$0
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Funding mix
By agency
NSF$3,573,228 · 12
By mechanism
—$3,573,228 · 12
Top collaborators
No co-investigators on record.
Grant awards (12)
Collaborative Research: Resolving the LGM ventilation age conundrum: New radiocarbon records from high sedimentation rate sites in the deep western Pacific$291,419
· FY2024 · GEO · contact PI
Was the deep Atlantic dominated by southern source waters during the LGM? A conservative view based on the oxygen isotopic ratio of benthic foraminifera$451,999
· FY2023 · GEO · contact PI
Do metalliferous sediments record mid-ocean ridge hydrothermal activity? Constraining the roles of iron oxidation rate and 230Th scavenging$442,790
· FY2020 · GEO · contact PI
Tracking Southern Ocean sea ice extent and frontal positions: Novel techniques based on oxygen isotope and Mg/Ca analyses of foraminifera$397,311
· FY2020 · GEO · contact PI
The Atlantic's role in ice age inception and termination: Assessing carbon storage and release with new Brazil Margin profiles from MIS 2 to MIS 6$433,137
· FY2018 · GEO · contact PI
EAGER: Anomalous submarine volcanism during glacial terminations: Exploring archives from the global mid-ocean ridge system$49,939
· FY2018 · GEO · contact PI
Millennial-scale atmospheric CO2 variability during the last deglaciation: Testing the biological pump hypothesis using upper ocean carbon isotope records$262,951
· FY2017 · GEO · contact PI
Collaborative Research: Sea level induced hydrothermal activity as a trigger for glacial terminations$279,999
· FY2016 · GEO · contact PI
Diagnosing the origin of isotopically light carbon in the South Atlantic during the last deglaciation: An oceanic or geologic source?$313,060
· FY2014 · GEO · contact PI
Collaborative Research: P2C2--Western Equatorial Pacific Rainfall during the Holocene - New Interannual Records from High Resolution Borneo Stalagmites$141,039
· FY2013 · GEO · contact PI
Collaborative Research: P2C2--Western Equatorial Pacific Rainfall during the Holocene - New Interannual Records from High Resolution Borneo Stalagmites$188,621
· FY2011 · GEO · contact PI
Antarctic Bottom Water Circulation during the Last Deglaciation: Quantitative Constraints from Stable Isotope Tracer Budgets$320,963
· FY2010 · GEO · contact PI