Search for Articles:
Title / Keyword
Author / Affiliation / Email
Journal
Article Type
 
 
Advanced Search
 
Section
Special Issue
Volume
Issue
Number
Page
 
5.3
2.4
Journals
Geosciences
Special Issues
Isotope Applied in Palaeogeography and Palaeoclimatology
share announcement

Isotope Applied in Palaeogeography and Palaeoclimatology

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Climate".

Deadline for manuscript submissions: closed (28 February 2022) | Viewed by 9150

Special Issue Editors

Dr. Tadeusz Peryt

E-Mail Website
Guest Editor
Polish Geological Institute – National Research Institute, 00–975 Warszawa, Poland
Interests: carbonate and evaporite sedimentology; stratigraphy; petroleum geology; isotope geology; palaeogeography; palaeoclimatology
Special Issues, Collections and Topics in MDPI journals
Dr. Marek Jasionowski

E-Mail Website
Guest Editor
Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975 vWarszawa, Poland
Interests: isotope geochemistry; sedimentology; diagenesis
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

This Special Issue of Geosciences aims to present recent advances in the application of stable isotopes in various fields of paleoclimate and paleogeography research. Past climates left their signatures in sediment records worldwide. In particular, this refers to the isotopic composition of elements that constitute biogenic and inorganic components of sedimentary rocks. For example, it is widely known that oxygen isotopes in ancient carbonates enable reconstruction of paleotemperatures and strontium isotopes are not only a tool for global stratigraphy but also provide information on paleoenvironmental conditions (marine versus non-marine). In general, stable isotope records are successfully used for investigating various ancient continental and marine settings. Knowing the various paleoclimatic parameters (temperature, humidity, etc.), one can infer paleogeography on a global or regional scale. Papers covering, but not limited to, the following topics are welcomed for submission to this Special Issue:

  • Paleothermometry – conventional and clumped oxygen isotopes;
  • Paleoaltimetry and evolution of landscapes using oxygen isotopes in authigenic minerals of continental sediments;
  • Carbon isotopes as paleoclimatic indicator;
  • Carbon isotopes in the global carbon cycle, its long-run changes and short-term disturbances in the geologic past – paleoclimate implications;
  • Isotopes (e.g. Si, Mg, Ca, Li, U) as a proxy for continental weathering and paleoclimate and paleogeographic reconstructions;
  • Isotopes of various elements in continental environments (lake sediments, paleosols, speleothems);
  • Isotopes as a proxy in paleogeographic reconstruction (ocean circulation, seaways connections, etc.).

Dr. Tadeusz Peryt
Dr. Marek Jasionowski
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Geosciences is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1800 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • e-Book format: Special Issues with more than 10 articles can be published as dedicated e-books, ensuring wide and rapid dissemination.

Further information on MDPI's Special Issue polices can be found here.

Published Papers (2 papers)

Download All Papers
Order results
Result details
Show export options expand_more Show export options expand_less
Select all
Export citation of selected articles as:

Research

Jump to: Review

15 pages, 3683 KiB  
Article
Oxygen Isotopes from Apatite of Middle and Late Ordovician Conodonts in Peri-Baltica (The Holy Cross Mountains, Poland) and Their Climatic Implications
by Wiesław Trela, Ewa Krzemińska, Karol Jewuła and Zbigniew Czupyt
Geosciences 2022, 12(4), 165; https://doi.org/10.3390/geosciences12040165 - 7 Apr 2022
Cited by 6 | Viewed by 3108
Abstract
This report provides oxygen isotopes from apatite of late Middle and Late Ordovician conodonts from the southern Holy Cross Mountains in south-eastern Poland. It was a unique time interval characterised by a significant change in the Ordovician climate, tectonic, and ocean chemistry. In [...] Read more.
This report provides oxygen isotopes from apatite of late Middle and Late Ordovician conodonts from the southern Holy Cross Mountains in south-eastern Poland. It was a unique time interval characterised by a significant change in the Ordovician climate, tectonic, and ocean chemistry. In the Middle and early Late Ordovician, the Holy Cross Mountains were located in the mid-latitude climatic zone at the southwestern periphery of Baltica; therefore, the δ18Oapatite values from this region provide new data on the 18O/16O budget in the Ordovician seawater reconstructed mainly from the tropical and subtropical realms. Oxygen isotopes from mixed conodont samples were measured using the SHRIMP IIe/MC ion microprobe in the Polish Geological Institute in Warsaw. The δ18Oapatite values range from 16.75‰VSMOW to 20.66‰VSMOW with an average of 18.48‰VSMOW. The oxygen isotopes from bioapatite of the studied section display an increasing trend, suggesting a progressive decrease in sea-surface temperature roughly consistent with an overall cooling of the Ordovician climate. Two distinctive positive excursions of δ18Oapatite have been reported in the upper Sandbian and middle Katian of the studied section and correlated with cooling events recognised in Baltica. They are interpreted as an isotope temperature proxy of climate changes triggered by a growing continental polar ice cap, but increased δ18Oapatite in the late Sandbian contradicts recently postulated climate warming during that time in subtropical Laurentia. Full article
(This article belongs to the Special Issue Isotope Applied in Palaeogeography and Palaeoclimatology)
►▼ Show Figures

Figure 1

Review

Jump to: Research

44 pages, 6161 KiB  
Review
Advances and Challenges in Palaeoenvironmental Studies Based on Oxygen Isotope Composition of Skeletal Carbonates and Phosphates
by Hubert Wierzbowski
Geosciences 2021, 11(10), 419; https://doi.org/10.3390/geosciences11100419 - 9 Oct 2021
Cited by 9 | Viewed by 5286
Abstract
Oxygen isotopes are widely used in palaeoenvironmental and palaeoclimatic studies as they record variations in the precipitation temperature of biogenic carbonates and phosphates. Problems associated with the preservation state of fossils, selection of the proper temperature equation, vital effects occurring during biomineralization, habitat [...] Read more.
Oxygen isotopes are widely used in palaeoenvironmental and palaeoclimatic studies as they record variations in the precipitation temperature of biogenic carbonates and phosphates. Problems associated with the preservation state of fossils, selection of the proper temperature equation, vital effects occurring during biomineralization, habitat effects of organisms as well as salinity, bathymetry and water circulation changes limit, however, the applicability of oxygen isotopes to reconstruction of ancient environmental settings. The progress of oxygen isotope studies, temperature calculations and ambiguities of the isotope record are discussed in this paper. The same applies to the methods of retrieving reliable temperature signals and the record of water chemistry changes based on well-preserved calcareous and phosphatic fossils. Sometimes neglected importance of sedimentological and faunistic data associated with sea-level changes and salinity variations is emphasised as an important tool for refinement of the temperature trends of epeiric sedimentary basins. In addition, published case datasets and new laboratory techniques, including micro-area and clumped isotope analyses, are presented to demonstrate examples and prospective ways of extension of the scope of palaeoenvironmental research. The provided information may be used in discussion and a critical review of published oxygen isotope data and their palaeoenvironmental interpretations. Full article
(This article belongs to the Special Issue Isotope Applied in Palaeogeography and Palaeoclimatology)
►▼ Show Figures

Figure 1

Show export options expand_more Show export options expand_less
Select all
Export citation of selected articles as:
 
Displaying articles 1-2
Back to TopTop