Hydrologic investigations in the Mammoth Corridor, Yellowstone National Park and vicinity, U.S.A.

Sorey, M.L.; Colvard, Elizabeth M.

doi:10.1016/s0375-6505(96)00041-7

Cited by 27 publications

(26 citation statements)

References 4 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…), dissolution Lopez et al (2017), Westaway (1993), Pentecost et al (1997), Kele et al (2011), De Filippis et al (2012, Özkul et al (2013), Van Noten et al (2013), Lebatard et al (2014), Claes et al (2015Claes et al ( , 2017aClaes et al ( , 2017b Sorey and Colvard (1997), Fouke et al (2000Fouke et al ( , 2003, Kharaka et al (2000), Chafetz and Guidry (2003), Kandianis et al (2008), Veysey et al (2008) Cipriani et al (1977), Barazzuoli et al (1988), Guo and Riding (1992, Pentecost (1995), Minissale et al (2002), Brogi et al (2007), Brogi and Capezzuoli (2008), Pedley (2009), Gandin and Capezzuoli (2014) Arp et al (2001Arp et al ( , 2010, Shiraishi et al (2008aShiraishi et al ( , 2008b, Brinkmann et al (2015) (continued on next page) et al, 2012; Nielsen et al, 2014). Lab and field studies report ACC phases found in close association with crystalline CaCO 3 (Jones and Peng, 2012a;Pedley, 2014) and/or organisms (cyanobacteria) or organic substances (Couradeau et al, 2012;Benzerara et al, 2014;Martignier et al, 2017).…”

Section: Tablementioning

confidence: 99%

What do we really know about early diagenesis of non-marine carbonates?

Boever

Brasier

Foubert

et al. 2017

Sedimentary Geology

View full text Add to dashboard Cite

Non-marine carbonate rocks including cave, spring, stream, calcrete and lacustrine-palustrine sediments, are susceptible to early diagenetic processes. These can profoundly alter the carbonate fabric and affect paleoclimatic proxies. This review integrates recent insights into diagenesis of non-marine carbonates and in particular the variety of early diagenetic processes, and presents a conceptual framework to address them. With ability to study at smaller and smaller scales, down to nanometers, one can now observe diagenesis taking place the moment initial precipitates have formed, and continuing thereafter. Diagenesis may affect whole rocks, but it typically starts in nano-and micro-environments. The potential for diagenetic alteration depends on the reactivity of the initial precipitate, commonly being metastable phases like vaterite, Ca-oxalates, hydrous Mg-carbonates and aragonite with regard to the ambient fluid. Furthermore, organic compounds commonly play a crucial role in hosting these early transformations. Processes like neomorphism (inversion and recrystallization), cementation and replacement generally result in an overall coarsening of the fabric and homogenization of the wide range of complex, primary microtextures. If early diagenetic modifications are completed in a short time span compared to the (annual to millennial) time scale of interest, then recorded paleoenvironmental signals and trends could still acceptably reflect original, depositional conditions. However, even compact, non-marine carbonate deposits may behave locally and temporarily as open systems to crystal-fluid exchange and overprinting of one or more geochemical proxies is not unexpected. Looking to the future, relatively few studies have examined the behaviour of promising geochemical records, such as clumped isotope thermometry and (non-conventional) stable isotopes, in well-constrained diagenetic settings. Ongoing and future in-vitro and in-situ experimental approaches will help to investigate and detangle sequences of intermediate, diagenetic products, processes and controls, and to quantify rates of early diagenesis, bridging a gap between nanoscale, molecular lab studies and the fossil field rock record of non-marine carbonates.

show abstract

Section: Tablementioning

confidence: 99%

What do we really know about early diagenesis of non-marine carbonates?

Boever

Brasier

Foubert

et al. 2017

Sedimentary Geology

View full text Add to dashboard Cite

show abstract

“…The hydrologic system at Angel Terrace is dynamic with multiple vents appearing, sealing, and reopening at a frequency of months to tens of years (Friedman, 1970;Bargar, 1978;Sorey and Colvard, 1997). Fouke et al (2000) characterize Angel Terrace deposits into multiple facies based on water temperature, chemistry, mineralogy, physical structure, and travertine accumulation rates.…”

Section: Site Description and Previous Studies Of Chemistry And Micromentioning

confidence: 99%

Lipid biomarkers and carbon-isotopes of modern travertine deposits (Yellowstone National Park, USA): Implications for biogeochemical dynamics in hot-spring systems

Zhang

Fouke

Bonheyo

et al. 2004

Geochimica et Cosmochimica Acta

View full text Add to dashboard Cite

“…(Sorey and Colvard, 1997). Helium isotopes are notably higher here at Mammoth Hot Springs than 15 km south within the NorrisMammoth tectonic corridor (Kennedy and others, 1985).…”

Section: 3mentioning

confidence: 97%

“…The pH of the discharged waters is typically about 6, but increases rapidly to about 8 as CO 2 is degassed ( fig. 14) at or near the surface (Sorey and Colvard, 1997;Kharaka and others, 2000 Fouke and others (2000) argue that the chemical variation of waters in Mammoth Hot Springs pools and drainages is almost entirely related to inorganic precipitation reactions, though the formation of travertine is accelerated by the physical presence of thermophilic bacteria, mainly cyanobacteria (Kandianis and others, 2008).…”

Section: Calcium-carbonate Watersmentioning

confidence: 99%