Pregled bibliografske jedinice broj: 1119216
Non-traditional stable isotope signatures in geological matrices as a tool for interpreting environmental changes – a review
Non-traditional stable isotope signatures in geological matrices as a tool for interpreting environmental changes – a review // Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society, 74/2 (2021), 177-187 doi:10.4154/gc.2021.12 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1119216 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Non-traditional stable isotope signatures in
geological matrices as a tool for interpreting
environmental changes – a review
Autori
Fiket, Željka ; Furdek Turk, Martina ; Ivanić, Maja ; Kniewald, Goran
Izvornik
Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society (1330-030X) 74/2
(2021);
177-187
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
non-traditional isotopes ; Ca and Mg ; Sr and Li ; transition metals ; geological matrices.
Sažetak
The development of new analytical techniques enabled the precise determination of the expanded set of stable isotopes and provided new insight into the existing geological issues. This review outlines recent studies of non-traditional isotope signatures in geological matrices, summarizing in one place new data for stable isotopes of Ca, Mg, Sr, Li, Ni, Cr, and Cu and their application in the interpretation of environmental processes. Although some of them, such as δ44Ca and δ26Mg, have been previously used to track changes in seawater chemistry throughout geological history, recent studies report their application as geochemical proxies of post- depositional processes. Similarly, isotopic signatures of strontium, previously used in radioactive isotope chronology, and δ7Li, used in tracing plate subduction and crust/mantle material cycling, found a new application in studies of weathering patterns. The use of δ53Cr and δ 65Cu isotope signatures, on the other hand, reflects their fractionation under different redox conditions, whereas δ60Ni, due to its adsorption and co-precipitation with sulfide species and Fe-Mn phases, is used in interpreting the contributions of different material sources. And while the isotopic signatures of all these elements indicate certain environmental conditions and processes (e.g. post-depositional processes, redox conditions, organic matter input, the contribution of sources, etc.), by combining them a more comprehensive insight into the investigated environment can be achieved.
Izvorni jezik
Engleski
Znanstvena područja
Interdisciplinarne prirodne znanosti
POVEZANOST RADA
Ustanove:
Institut "Ruđer Bošković", Zagreb
Profili:
Maja Ivanić
(autor)
Goran Kniewald
(autor)
Željka Fiket
(autor)
Martina Furdek Turk
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus