Methods to Investigate Source-to-Sink Systems


ESRs in the field and in the lab. The sample processing starts by describing, counting, measuring, sampling, and investigating in the field. Samples are then taken to the laboratory for analytical work. Keep up with future posts to see the field and laboratory results!

Much like building a complex puzzle, multiple components come together to foster an understanding of the evolution of S2S systems at various temporal and spatial scales. Some of these components are (1) understanding the major processes and fluvial dynamics acting on the system, (2) recognizing the changes or signals in the sedimentary record, (3) deciphering the environment necessary to produce a given signal within the record, and (4) contemplating other dynamics that would change the expression of an environmental event in the final rock/sediment record. Thus, studying S2S systems often requires an integration of research methods and the collaboration of specialists across different fields. 

 

Pieces of the puzzle; Fostering understanding of source to sink systems through multidisciplinary methods. 

1. Fieldwork

Several field observation methods are essential in source-to-sink analysis. Here, we describe sedimentology, stratigraphy, and geomorphology as three of the most essential research methods. Other methods are generally based on their concepts and principles. Therefore, understanding their basics is fundamental for the application and interpretation of any method.

1.1 Sedimentology 

Sedimentology is concerned with describing, classifying, and understanding the origin of sedimentary rocks. It helps us to understand the processes of formation, transportation, deposition, and diagenesis. The main goal is to interpret ancient environmental conditions of S2S systems by gathering fieldwork data from outcrops in terms of constituents, textures, structures, and fossils.


(A) Sedimentological and gamma-ray logs for a geological section studied and (B) sedimentological logging in the field in southwest Germany (modified from Palermo et al., 2010). (C) Basic template sheet for constructing graphic sedimentary logs (Nichols, G. 1999).


1.2 Stratigraphy 


Stratigraphy studies the accumulation and distribution of layered rocks denominated strata in space. An important principle is Steno’s Law of Superposition, which says, “younger strata overlie older strata”. These principles in combination with interpretation of physical, biological and chemical properties of sedimentary layers help to define surfaces and units based on the vertical changes of those properties in the stratigraphic succession. There are several sub-disciplines of stratigraphy and each one focuses on investigating a set of properties. For instance, lithostratigraphy focuses on changes in lithology (physical properties like color, grain size, texture, composition), biostratigraphy focuses on changes in fossil content and requires expertise in paleontology (the science that studies life forms appearing, living, and being extinct at some point). It is also used for dating (see 3.2 Geochronology).

1.3. Geomorphology 

Geomorphology investigates landforms, their processes, shapes, and sediments at the surface of the Earth. This observation includes looking at landscapes to understand how the Earth's surface processes, such as air, water, and ice, can shape the landscape. Most of the Earth's surface processes are changing the landscape very slowly but some are very rapid like landslides or floods. Advancements in remote sensing from satellites and GIS mapping such that we can see from Google Earth allow geomorphologists or even amateurs to understand the landscapes on a global scale.


Landsat image of northeastern Chad and its interpretation which is observed from Google Earth (Griffin, 2006).

2. Laboratory Analyses 

Once field data has been collected and sorted in the field, analytical work can be performed in the laboratory setting. The laboratory methods are very specific and depend on the target of study, but in general, they involve the chemical and physical treating of rocks or minerals. 


2.1 Mineralogy


During denudation, rocks are broken into sediments, and the material further “decomposes” and forms secondary minerals. In our systems, these newly formed minerals are clay minerals. The clay mineral composition reflects the environmental conditions during its formation, and thus the climatic conditions can be estimated. The process starts with separating the clay-sized particles from the coarser grains in the laboratory. The unaltered minerals and clasts in the sediment also give insight into the type of rocks from which the sediment originates (e.g., is it volcanic, does it originate from a continent or an oceanic crust?). This is based on the fact that rocks with a specific composition will generate sediments of similar composition. For example, if we have granite (an igneous rock with high feldspar and quartz content) after weathering and erosion we will most likely get feldspathic and quartz-rich sandstones, which is different from what we will get if we erode a basalt (volcanic rock) in the first place. The provenance of sediment will be examined further with geochronological methods afterward (see 2.3 Geochronology).




Clay-sized fraction separation in the laboratory using Stoke’s law.


2.2 Geochemistry

Geochemical analyses are broad, and the applied methods depend on the target material. This can range from the whole rock composition of the samples (X-ray fluorescence analyses), down to the minor and trace elements (ICP MS analyses). Stable isotope geochemistry, for example, can provide diverse information on the sediment routing system, including changes in the precipitation regime, in the paleoelevation, or even in the biological activity, which is expressed in the fractionation of heavy vs. light isotopes.

2.3 Geochronology

Geochronology means determining the age of certain Earth material, for example, a rock, a fossil, or even sediment and soil. Thus the sediment will be connected to a geological event, e.g., the eruption of a volcano, the age of a mountain belt, or even an extinction event. There are two types of age-determination of earth materials:
  • Relative dating does not provide a precise age, it just indicates if a specific rock or fossil is younger/older than others. Thus, this dating method relies on the Superposition Law (see 1.2 Stratigraphy).
  • Radiometric dating gives a precise age (plus measurement of its uncertainty, e.g. 21.7 ± 0.8 Ma).  It calculates an age in years for geologic materials by measuring the presence of radioactive elements, e.g., C14, K/Ar, etc.

3. Landscape Evolution Modelling (LEM) 

LEMs have revolutionized the way geoscientists can compute the entire landscape over millions of years in less time than it would take to brew a cup of coffee. LEMs rely upon and illustrate the various relationships between geomorphic variables (such as terrain slope, sediment flux, watershed area, and more). Changes from the source to the sink due to climatic, tectonic, and lithologic events can be analyzed using a LEM. Findings derived through LEMs are validated with real-world field observations and have a vast breadth of applications. 


Landscape Evolution Model (Fastscape). Example of a Source to Sink system (Prof. Dr. Jean Braun GFZ Potsdam).


As we have seen there are several methods to study source-to-sink systems and their components, and there are even plenty more that we have not covered yet. It is necessary to bear in mind that the most important thing is to understand how we integrate abundant data and complement different research methods in order to get the best picture of them.



If you have any questions about the methods described to study source-to-sink or do you want to know more about other methods, please leave a comment below! Thank you for reading and see you next month for the next post!



References:

  • Griffin, D. (2006). The late Neogene Sahabi rivers of the Sahara and their climatic and environmental implications for the Chad Basin. Journal of the Geological Society, London, Vol. 163, pp. 905-921. https://doi.org/10.1144/0016-76492005-049

  • Nichols, G. (1999). Sedimentology and stratigraphy. Oxford: Blackwell Science.

  • Palermo, D., Aigner, T., Nardon, S., & Blendinger, W. (2010). Three-dimensional facies modeling of carbonate sand bodies: Outcrop analog study in an epicontinental basin (Triassic, southwest Germany). American Association of Petroleum Geologists Bulletin, 94(4), 475–512. https://doi.org/10.1306/08180908168

  • Posamentier, H. W., & George P Allen. (1999). Siliciclastic sequence stratigraphy: Concepts and applications: SEPM Concepts in Sedimentology and Paleontology. In Concepts in Sedimentology and Paleontology (Issue 7).

Location: Geneva, Switzerland

Comments

Post a Comment

Popular posts from this blog

What is a Source-to-Sink System?

Image
A  source-to-sink analysis is a method in sedimentary geology that integrates the studies of an entire sedimentary system from its upstream source in the continental area to the ultimate depositional sink , most commonly on deep basin s, in a process that can take from thousands to millions of years to be completed.   Source-to-sink system schematic (modified from Martinsen et al., 2010). There are three main elements in the source-to-sink system, source, transfer zone, and sink.       1) Source Source area in the source-to-sink system is in the continental realm where the main erosional processes occur. The erosion process in the source area is mainly driven by slow processes which can take millions of years: tectonics and climate. Tectonics generates high relief structures like mountains while climatic factors like precipitation bring water down the mountains. Hence, more sediment supply can be provided from the source area.  During the erosion pro...
Read more

What is a “Slow” Process in a Source-to-Sink System?

Image
The timescale of geological processes is very extensive. “Fast” processes like earthquakes, storms, or tides last from a couple of minutes to weeks. “Slow” processes, like orogenic uplifts or continent break-ups on the contrary can take up to millions of years (Fig. 1). In this post we will look into these slow processes in the context of the source-to-sink approach, introducing some concepts that provide a useful framework to understand the dynamics of these long processes in sedimentary systems. Figure 1. Temporal scale showing the differences in terms of duration of several geological processes as well as the common tools used to measure them. Bear in mind that the scale is logarithmic. Modified from Romans et al ., 2016. To understand slow geological processes in the context of source-to-sink analysis, we first have to understand the concept of steady-state topography. There are two major processes that drive topography inside a catchment (Fig. 2), one that creates positive rel...
Read more

ITN opportunities: Summer-schools (Part 1)

Image
Since the beginning of the project, multiple interesting opportunities have been presented to us. We would travel each year to conferences like EGU, present and convene, introduce ourselves to the scientific community, make connections, go on different secondments according to our needs during our doctoral studies, but also opportunities to meet each other during the years, with one important meeting for everyone each year: the summer schools. It was the only time where all of us were together for multiple weeks, to exchange, learn and evolve in our respective fields, but also learn in more detail about the subjects of our colleagues. Some cooperation started between us thanks to those summer schools. To cite some, Marine and Philémon during Dragonstone, in Spain in 2021 or Amanda, Rocío, Nahin, Ariel and Marine during Inside Africa, in Namibia in 2023. Thus, it is appropriate to present, through this blog, an overview about the summer schools. We could talk about each of them for da...
Read more