Mineralogy as a potential driver of irregular radiocarbon patterns among Icelandic fluvial carbon pools

Abstract Fluvial export of organic carbon (OC) from the terrestrial biosphere to the ocean forms a key component of the global carbon cycle. Carbon sources and transformations along the land–ocean aquatic continuum are dynamic with a complex interplay between particulate and dissolved organic and inorganic carbon pools (POC, DOC, DIC). Radiocarbon dating serves as a valuable tool, providing crucial insights into turnover and residence times within these pools. However, the myriad of carbon sources, including ancient ‘petrogenic’ OC from sedimentary rocks or freshly assimilated OC derived from aquatic in-situ production, makes it challenging to interpret 14 C signatures in the context of terrestrial biospheric OC turnover and residence times. Icelandic rivers and streams offer an opportunity to examine biospheric carbon dynamics due to the virtual absence of petrogenic OC (e.g., shales, carbonates) in underlying bedrock. Our study of 43 rivers and streams, collectively draining approximately 42% of Iceland’s surface, revealed that radiocarbon signatures of POC largely align with global river patterns but lacked the presence of significantly old ( 14 C-depleted) carbon likely reflecting the absence of ancient petrogenic OC. In contrast, DOC tended to be older compared to global rivers and the corresponding POC and DIC pools in Icelandic rivers. These observations challenge the paradigm that riverine POC generally exhibits longer turnover and residence times than DOC. After excluding other potential factors, we argue that this apparent age inversion among carbon pools in Icelandic rivers may reflect retention of DOC prior to its release to the aquatic continuum through interactions with high surface area minerals prevalent in the volcanic soils of Iceland. This finding may be relevant for other fluvial systems draining volcanic bedrock and have broader implications regarding biospheric OC dynamics in rivers and streams globally.

Authors

Institutions

Publication Details

Journal
Environmental Research Letters
Published
2024-12-31
DOI
https://doi.org/10.1088/1748-9326/ada45c
Citations
1
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.38

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Mineralogy as a potential driver of irregular radiocarbon patterns among Icelandic fluvial carbon pools

Timothy I. Eglinton, Negar Haghipour, Stephan Wartenweiler, Julie Lattaud et al.
1 citations
Environmental Research Letters
Geology and Paleoclimatology Research
0.38
article

Mineralogy as a potential driver of irregular radiocarbon patterns among Icelandic fluvial carbon pools

Timothy I. Eglinton, Negar Haghipour, Stephan Wartenweiler, Julie Lattaud, Lisa Bröder, Nora Gallarotti
article en
1 citations

Abstract

Abstract Fluvial export of organic carbon (OC) from the terrestrial biosphere to the ocean forms a key component of the global carbon cycle. Carbon sources and transformations along the land–ocean aquatic continuum are dynamic with a complex interplay between particulate and dissolved organic and inorganic carbon pools (POC, DOC, DIC). Radiocarbon dating serves as a valuable tool, providing crucial insights into turnover and residence times within these pools. However, the myriad of carbon sources, including ancient ‘petrogenic’ OC from sedimentary rocks or freshly assimilated OC derived from aquatic in-situ production, makes it challenging to interpret 14 C signatures in the context of terrestrial biospheric OC turnover and residence times. Icelandic rivers and streams offer an opportunity to examine biospheric carbon dynamics due to the virtual absence of petrogenic OC (e.g., shales, carbonates) in underlying bedrock. Our study of 43 rivers and streams, collectively draining approximately 42% of Iceland’s surface, revealed that radiocarbon signatures of POC largely align with global river patterns but lacked the presence of significantly old ( 14 C-depleted) carbon likely reflecting the absence of ancient petrogenic OC. In contrast, DOC tended to be older compared to global rivers and the corresponding POC and DIC pools in Icelandic rivers. These observations challenge the paradigm that riverine POC generally exhibits longer turnover and residence times than DOC. After excluding other potential factors, we argue that this apparent age inversion among carbon pools in Icelandic rivers may reflect retention of DOC prior to its release to the aquatic continuum through interactions with high surface area minerals prevalent in the volcanic soils of Iceland. This finding may be relevant for other fluvial systems draining volcanic bedrock and have broader implications regarding biospheric OC dynamics in rivers and streams globally.

Environmental Research LettersVol. 20(2)
Planetary Science Institute (US), University of Basel (CH), ETH Zurich (CH), École Polytechnique Fédérale de Lausanne (CH)
National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Life below water
Openalex Percentile: Top 37%
Geology and Paleoclimatology Research
0.38
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.