Zn and Cd isotopes as proxies for geochemical change in Mesozoic oceans
<p>Mesozoic Oceanic Anoxic Events (OAEs) are characterised by the widespread burial of organic-rich sediments and the spread of low-oxygen marine environments. These intervals represent some of most extreme perturbations to global climate, environment, and ocean chemistry in Earth’s history...
Main Author: | Sweere, T |
---|---|
Other Authors: | Porcelli, D |
Format: | Thesis |
Published: |
2018
|
Similar Items
-
Oceanic cycling of rare earth elements and the application of Nd isotopes to assess changes in Mesozoic ocean circulation
by: Zheng, X
Published: (2016) -
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica
by: Hendry, K, et al.
Published: (2008) -
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica
by: Hendry, K, et al.
Published: (2008) -
A bottom-up perspective on ecosystem change in Mesozoic oceans
by: Knoll, Andrew H., et al.
Published: (2018) -
Systematic thallium isotope variation in Fe-Mn crusts: A proxy for changes in ocean chemistry?
by: Nielsen, S, et al.
Published: (2007)