4.2 Article

Testing commonly used X-ray fluorescence core scanning-based proxies for organic-rich lake sediments and peat

Journal

BOREAS
Volume 45, Issue 1, Pages 180-189

Publisher

WILEY
DOI: 10.1111/bor.12145

Keywords

-

Funding

  1. Swedish Research Council [621-2008-2855]
  2. Royal Thai Government Scholarship (DPST Programme)

Ask authors/readers for more resources

X-ray fluorescence (XRF) core scanning has become widely available for geological studies during the last decade. The data obtained from XRF core scanning, however, may be strongly influenced by the amount of organic matter, water content, density and porosity of the sediment matrix. In this study we discuss the usefulness of XRF core scanning to distinguish different kinds of organic-rich sediments and peat based on examples from tropical Lakes Kumphawapi and Nong Leng Sai in Thailand. We examined how sedimentary factors influence XRF core scanning analyses by comparing elemental and scattering ratios to lithological changes and quantitative LOI, TOC, biogenic silica (BSi) and grain-size values. Our comparison suggests that the (inc/coh) scattering ratio is of limited use as an indicator for variations in LOI and TOC in peaty gyttja or peat. In Lake Kumphawapi's sediments, Si/Ti ratios reflect clastic input associated with grain-size variations rather than BSi contents. The Ti-normalized ratios of Si, Zr, Sr, K and Rb are linked to mineral input and associated grain-size variations. We conclude that XRF core scanning of organic-rich tropical lake sediments and peat is useful to infer palaeoenvironmental conditions. However, XRF core scanning data does not stand-alone and needs to be underpinned by additional proxies.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.2
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Geography, Physical

New insights from XRF core scanning data into boreal lake ontogeny during the Eemian (Marine Isotope Stage 5e) at Sokli, northeast Finland

Malin E. Kylander, Anna Plikk, Johan Rydberg, Ludvig Lowemark, J. Sakari Salonen, Maria Fernandez-Fernandez, Karin Helmens

QUATERNARY RESEARCH (2018)

Article Geosciences, Multidisciplinary

Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary

Stefanie Kaboth-Bahr, Andre Bahr, Christian Zeeden, Samuel Toucanne, Frederique Eynaud, Francisco Jimenez-Espejo, Ursula Rohl, Oliver Friedrich, Joerg Pross, Ludvig Lowemark, Lucas J. Lourens

GEOPHYSICAL RESEARCH LETTERS (2018)

Article Geography, Physical

Changes in sea ice cover and ice sheet extent at the Yermak Plateau during the last 160 ka - Reconstructions from biomarker records

A. Kremer, R. Stein, K. Fahl, Z. Ji, Z. Yang, S. Wiers, J. Matthiessen, M. Forwick, L. Lowemark, M. O'Regan, J. Chen, I. Snowball

QUATERNARY SCIENCE REVIEWS (2018)

Article Geography, Physical

What caused the cultural hiatus in the Iron-Age Kiwulan Site, northeastern Taiwan?

Jyh-Jaan Steven Huang, Kuo-Yen Wei, Ludvig Lowemark, Sheng-Rong Song, Chih-Kai Chuang, Tien-Nan Yang, Meng-Yang Lee, Yu-Be Chen, Chorng-Shern Horng, Kuo-Hang Chen, Teh-Quei Lee

QUATERNARY INTERNATIONAL (2019)

Article Geography, Physical

Practical guidelines and recent advances in the Itrax XRF core-scanning procedure

Ludvig Lowemark, Menno Bloemsma, Ian Croudace, J. Stephen Daly, Robin J. Edwards, Pierre Francus, Jennifer M. Galloway, Braden R. B. Gregory, Jyh-Jaan Steven Huang, Anna F. Jones, Malin Kylander, Ludvig Lowemark, Yangbing Luo, Suzanne Maclachlan, Christian Ohlendorf, R. Timothy Patterson, Christof Pearce, Jorn Profe, Eduard G. Reinhardt, Christian Stranne, Rik Tjallingii, Jonathan N. Turner

QUATERNARY INTERNATIONAL (2019)

Article Geography, Physical

Deciphering ∼45.000 years of Arctic Ocean lithostratigraphic variability through multivariate statistical analysis

Stefanie Kaboth-Bahr, Vianney Denis, Chih-Chieh Su, Matt O'Regan, Richard Gyllencreutz, Martin Jakobsson, Ludvig Lowemark

QUATERNARY INTERNATIONAL (2019)

Editorial Material Geography, Physical

High resolution XRF core scanners: A key tool for the environmental and palaeoclimate sciences

Ian W. Croudace, Ludvig Lowemark, Rik Tjallingii, Bernd Zolitschka

QUATERNARY INTERNATIONAL (2019)

Article Geography, Physical

Current perspectives on the capabilities of high resolution XRF core scanners

Ian W. Croudace, Ludvig Lowemark, Rik Tjallingii, Bernd Zolitschka

QUATERNARY INTERNATIONAL (2019)

Article Multidisciplinary Sciences

Rapid assessment of heavy metal pollution using ion-exchange resin sachets and micro-XRF core-scanning

Jyh-Jaan S. Teven Huang, Sheng-Chi Lin, Ludvig Lowemark, Sofia Ya Hsuan Liou, Queenie Chang, Tsun-Kuo Chang, Kuo-Yen Wei, Ian W. Croudace

SCIENTIFIC REPORTS (2019)

Article Geosciences, Multidisciplinary

Stratigraphic Occurrences of Sub-Polar Planktic Foraminifera in Pleistocene Sediments on the Lomonosov Ridge, Arctic Ocean

Matt O'Regan, Helen K. Coxall, Thomas M. Cronin, Richard Gyllencreutz, Martin Jakobsson, Stefanie Kaboth, Ludvig Lowemark, Steffen Wiers, Gabriel West

FRONTIERS IN EARTH SCIENCE (2019)

Article Multidisciplinary Sciences

Rainfall variations in central Indo-Pacific over the past 2,700 y

Liangcheng Tan, Chuan-Chou Shen, Ludvig Lowemark, Sakonvan Chawchai, R. Lawrence Edwards, Yanjun Cai, Sebastian F. M. Breitenbach, Hai J. Cheng, Yu-Chen Chou, Helmut Duerrast, Judson W. Partin, Wenju Cai, Akkaneewut Chabangborn, Yongli Gao, Ola Kwiecien, Chung-Che Wu, Zhengguo Shi, Huang-Hsiung Hsu, Barbara Wohlfarth

PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2019)

Article Geosciences, Multidisciplinary

Multi-proxy evidence for rapidly shifting sediment sources to the Taiwan Western Foreland Basin at the Miocene-Pliocene transition

Amy Hsieh, Shahin E. Dashtgard, Pei-Ling Wang, Chorng-Shern Horng, Chih-Chieh Su, Andrew T. Lin, Romain Vaucher, Ludvig Lowemark

Summary: The Taiwan Western Foreland Basin was traditionally believed to have received sediment mainly from Eurasia until the late Pliocene-early Pleistocene. However, new research indicates that major sediment contributions from Taiwan occurred much earlier, and were closely related to the uplift and initial emergence of the Taiwan orogen. This study demonstrates that the Taiwan orogen became a significant source of sediment to the Western Foreland Basin during the Miocene-Pliocene transition, about two million years earlier than previously recognized.

BASIN RESEARCH (2023)

Article Environmental Sciences

Disentangling the impact of anthropogenic and natural processes on the environment in a subtropical subalpine lake catchment in northeastern Taiwan over the past 150 years

Tsai-Wen Lin, Stefanie Kaboth-Bahr, Andre Bahr, Kweku Afrifa Yamoah, Chih-Chieh Su, Liang-Chi Wang, Pei-Ling Wang, Ludvig Loewemark

Summary: Human activities have caused significant changes in sedimentation processes and vegetation cover in lake catchments. However, the time needed for anthropogenically disturbed areas to return to their natural state through environmental protection programs is still uncertain. This study focuses on the Cueifong Lake catchment in Taiwan and uses a multi-proxy approach to investigate major environmental disturbances such as logging and forest fires. The results suggest that it may take more than 50 years for the sedimentary regime to fully recover from logging activities, while the vegetation composition may shift irreversibly towards an algae-dominant environment.

SCIENCE OF THE TOTAL ENVIRONMENT (2023)

Article Geosciences, Multidisciplinary

Influence of a Rapidly Uplifting Orogen on the Preservation of Climate Oscillations

Amy I. I. Hsieh, Romain Vaucher, Ludvig Lowemark, Shahin E. Dashtgard, Chorng-Shern Horng, Andrew T. T. Lin, Christian Zeeden

Summary: This study evaluates how the evolving Taiwan orogen influences the preservation of astronomical climate forcing in the shallow-marine sedimentary strata of the Taiwan Western Foreland Basin. The findings show that long-term astronomical cycles were poorly preserved during the early stages of increased East Asian Summer Monsoon due to wave reworking. However, from 5.4 to 3.15 Ma, the development of the basin and the protection provided by Taiwan enhanced the preservation of astronomical climate variability.

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY (2023)

Article Geology

Storm-flood-dominated delta succession in the Pleistocene Taiwan Strait

Romain Vaucher, Antoine Dillinger, Amy I. Hsieh, Wen-Rong Chi, Ludvig Lowemark, Shahin E. Dashtgard

Summary: This paper reports on the sedimentary succession of the Pleistocene Cholan Formation in Taiwan, which provides insights into the deposition processes of storm-flood delta successions. The study reveals the occurrence of tropical cyclone beds and post-depositional deformation features, and highlights the differences in sedimentary structures compared to other storm-flood delta successions.

DEPOSITIONAL RECORD (2023)

No Data Available