Award Abstract # 2051199
Collaborative Research: Trace Elements in Pyrite?Validation and Calibration of a Novel Paleoenvironmental Proxy

NSF Org: EAR
Division Of Earth Sciences
Recipient: CENTRAL MICHIGAN UNIVERSITY
Initial Amendment Date: June 21, 2021
Latest Amendment Date: June 21, 2021
Award Number: 2051199
Award Instrument: Standard Grant
Program Manager: Jonathan G Wynn
jwynn@nsf.gov
 (703)292-4725
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: June 15, 2021
End Date: May 31, 2025 (Estimated)
Total Intended Award Amount: $244,516.00
Total Awarded Amount to Date: $244,516.00
Funds Obligated to Date: FY 2021 = $244,516.00
History of Investigator:
  • Anthony Chappaz (Principal Investigator)
    anthony.c@cmich.edu
Recipient Sponsored Research Office: Central Michigan University
119 BOVEE UNIVERSITY CTR
MOUNT PLEASANT
MI  US  48858-3854
(989)774-6467
Sponsor Congressional District: 02
Primary Place of Performance: Central Michigan University
Brooks 313A, EAS
Mt. Pleasant
MI  US  48858-4679
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): JJDYK36PRTL5
Parent UEI:
NSF Program(s): Geobiology & Low-Temp Geochem
Primary Program Source: 01002122DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 7295, 7298
Program Element Code(s): 729500
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Life in the oceans is often limited by the availability of nutrients, such as nitrogen and phosphorus. Other elements occurring in far lower abundances are also bioessential and potentially limiting?particularly trace metals such as iron and molybdenum. These metals are co-factors in many biological processes, and their distributions through time and space are strongly coupled to oxygen levels in the oceans; weathering of the continents; evolving atmospheric composition; and biological evolution. All of these factors tie intimately to climate change as a critical driver and consequence of metal cycling on land and in the oceans. Yet, despite extensive study of metals in modern and ancient oceans, basic gaps remain in our knowledge because of inadequate testing of certain chemical methods, particularly in the modern oceans. These methods, once refined, would allow for more confident exploration of a vast array of past conditions at Earth?s surface?far beyond those seen today. From that reinforced vantage, researchers can begin to imagine more rigorously and comprehensively what may lie in our future. One of the most promising methods for ?time travel? through Earth?s evolving oceans is elemental analysis of pyrite, an iron sulfide mineral common today and in the past that may provide easily accessible and highly preservable historical archives. Surprisingly, despite the advantages that may lie with this approach and hints of success already, no previous effort has attempted to validate and calibrate the pyrite tracer in modern oceans where present environmental conditions, local and global, can be tied directly to the composition of the mineral. This study is the first comprehensive investigation of these relationships in modern systems, strengthened by targeted experiments and novel analytical techniques. The principal expected outcome is an improved understanding of the controls and consequences of change at Earth?s surface as expressed in evolving ocean chemistry?past, present, and future?and the cause-and-effect relationships with co-evolving life.

Many studies are now using a technique called laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) to measure trace metal contents of pyrite as a tracer for past marine conditions, and the initial results are encouraging. That said, there is still little mechanistic understanding of how and when trace elements are incorporated into pyrite and how these patterns and controls vary across environmental gradients. These uncertainties weaken their utility. The relationships among local controls and the capture of potentially global signals remain largely unknown. Thus motivated, this study is designed around a two-pronged approach: (1) sampling in five classic, well-studied modern marine environments with a well characterized diversity of primary environmental conditions and (2) complementary, carefully conceived laboratory simulations designed to provide unprecedented insight into the mechanisms of trace metal uptake by iron sulfide minerals and their sensitivity to environmental backdrops. The ultimate goal is to expose the strengths and weaknesses of the proxy and best practices while revealing new opportunities, such as the possibility of tracking the availability of bioessential trace metals in the ancient deep biosphere. Plans include analyzing pore waters and sediments from diverse settings in modern oceans and interpreting those data within the framework of experimental results to reveal how trace metal content scales with conditions in the surrounding environment. The utility of the approach will be explored further using novel, highly sophisticated analytical methods applied at high resolution to characterize experimental and natural samples. This will be the first systematic study that correlates pyrite metal contents with metal availability in surrounding fluids and relates such data more generally to the wide range of environmental parameters and proxies often included in studies of Earth?s ancient biosphere. The impacts of this study will extend broadly through outreach opportunities targeting middle and high school students and UCR undergraduates placed in the Lyons lab, while championing diversity and inclusion at all levels. That community footprint will be expanded through a recurring public lecture series and an on-campus science festival presented entirely in Spanish, among other already tested community-directed efforts. At CMU, plans include a geochemical study at two middle schools in Flint (MI) emphasizing water quality and use of those data to construct a new, much-needed community-driven water quality database for Flint.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Bian, Leibo and Chappaz, Anthony and Schovsbo, Niels H. and Sanei, Hamed "A new vanadium species in black shales: Updated burial pathways and implications" Geochimica et Cosmochimica Acta , v.338 , 2022 https://doi.org/10.1016/j.gca.2022.09.035 Citation Details
Bian, Leibo and Chappaz, Anthony and Schovsbo, Niels H and Wang, Xiaomei and Zhao, Wenzhi and Sanei, Hamed "A 20-million-year reconstruction to decipher the enigmatic Cambrian extinction Ordovician biodiversification transition" Earth and Planetary Science Letters , v.612 , 2023 https://doi.org/10.1016/j.epsl.2023.118170 Citation Details
Bian, Leibo and Chappaz, Anthony and Schovsbo, Niels Hemmingsen and Nielsen, Arne Thorshøj and Sanei, Hamed "High mercury enrichments in sediments from the Baltic continent across the late Cambrian: Controls and implications" Chemical Geology , v.599 , 2022 https://doi.org/10.1016/j.chemgeo.2022.120846 Citation Details
Bian, Leibo and Chappaz, Anthony and Wang, Xiaomei and Amouroux, David and Schovsbo, Niels Hemmingsen and Zheng, Xiaowei and Sanei, Hamed "Improving Mercury Systematics With Molybdenum and Vanadium Enrichments: New Insights From the CambrianOrdovician Boundary" Geophysical Research Letters , v.51 , 2024 https://doi.org/10.1029/2023GL107188 Citation Details
Bian, Leibo and Schovsbo, Niels H. and Chappaz, Anthony and Rudra, Arka and Xu, Jin and Luo, Qingyong and Sanei, Hamed "Paleoenvironmental Reconstruction and Organic Matter Accumulation of the Lower Cambrian Qiongzhusi Formation in the Sichuan Basin, South China" ACS Earth and Space Chemistry , v.6 , 2022 https://doi.org/10.1021/acsearthspacechem.2c00224 Citation Details
Guida, Carolina and Ramothe, Vivien and Chappaz, Anthony and Simonnin, Pauline and Rosso, Kevin M and Ding, Rong-Rong and Prieur, Damien and Scheinost, Andreas C and Charlet, Laurent "Revisiting Selenium Interactions with Pyrite: From Adsorption to Coprecipitation" ACS Earth and Space Chemistry , v.8 , 2024 https://doi.org/10.1021/acsearthspacechem.3c00219 Citation Details

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