Bedrock Weathering Controls on Terrestrial Carbon-Nitrogen-Climate Interactions
Dass, Pawlok ; Houlton, Benjamin Z. ; Wang, Yingping ; Wårlind, David LU
and Morford, Scott
(2021)
In Global Biogeochemical Cycles
35(10).
- Abstract
Anthropogenic nitrogen deposition is widely considered to increase CO2 sequestration by land plants on a global scale. Here, we demonstrate that bedrock nitrogen weathering contributes significantly more to nitrogen-carbon interactions than anthropogenic nitrogen deposition. This working hypothesis is based on the introduction of empirical results into a global biogeochemical simulation model over the time period of the mid-1800s to the end of the 21st century. Our findings suggest that rock nitrogen inputs have contributed roughly 2–11 times more to plant CO2 capture than nitrogen deposition inputs since pre-industrial times. Climate change projections based on RCP 8.5 show that rock nitrogen inputs and biological... (More)
Anthropogenic nitrogen deposition is widely considered to increase CO2 sequestration by land plants on a global scale. Here, we demonstrate that bedrock nitrogen weathering contributes significantly more to nitrogen-carbon interactions than anthropogenic nitrogen deposition. This working hypothesis is based on the introduction of empirical results into a global biogeochemical simulation model over the time period of the mid-1800s to the end of the 21st century. Our findings suggest that rock nitrogen inputs have contributed roughly 2–11 times more to plant CO2 capture than nitrogen deposition inputs since pre-industrial times. Climate change projections based on RCP 8.5 show that rock nitrogen inputs and biological nitrogen fixation contribute 2–5 times more to terrestrial carbon uptake than anthropogenic nitrogen deposition though year 2101. Future responses of rock N inputs on plant CO2 capture rates are more signficant at higher latitudes and in mountainous environments, where geological and climate factors promote higher rock weathering rates. The enhancement of plant CO2 uptake via rock nitrogen weathering partially resolves nitrogen-carbon discrepancies in Earth system models and offers an alternative explanation for lack of progressive nitrogen limitation in the terrestrial biosphere. We conclude that natural N inputs impart major control over terrestrial CO2 sequestration in Earth’s ecosystems.
(Less)
- author
- Dass, Pawlok
; Houlton, Benjamin Z.
; Wang, Yingping
; Wårlind, David
LU
and Morford, Scott
- organization
- publishing date
- 2021-10
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- bedrock weathering, carbon cycle, nitrogen cycle, nitrogen deposition, nitrogen fixation, nitrogen limitation
- in
- Global Biogeochemical Cycles
- volume
- 35
- issue
- 10
- article number
- e2020GB006933
- publisher
- American Geophysical Union (AGU)
- external identifiers
-
- scopus:85118219098
- ISSN
- 0886-6236
- DOI
- 10.1029/2020GB006933
- language
- English
- LU publication?
- yes
- additional info
- Publisher Copyright: © 2021. The Authors.
- id
- c9735b21-c6ef-4b89-8ceb-93d11aa0575a
- date added to LUP
- 2021-11-13 09:40:08
- date last changed
- 2023-03-08 02:26:32
@article{c9735b21-c6ef-4b89-8ceb-93d11aa0575a,
abstract = {{<p>Anthropogenic nitrogen deposition is widely considered to increase CO<sub>2</sub> sequestration by land plants on a global scale. Here, we demonstrate that bedrock nitrogen weathering contributes significantly more to nitrogen-carbon interactions than anthropogenic nitrogen deposition. This working hypothesis is based on the introduction of empirical results into a global biogeochemical simulation model over the time period of the mid-1800s to the end of the 21st century. Our findings suggest that rock nitrogen inputs have contributed roughly 2–11 times more to plant CO<sub>2</sub> capture than nitrogen deposition inputs since pre-industrial times. Climate change projections based on RCP 8.5 show that rock nitrogen inputs and biological nitrogen fixation contribute 2–5 times more to terrestrial carbon uptake than anthropogenic nitrogen deposition though year 2101. Future responses of rock N inputs on plant CO<sub>2</sub> capture rates are more signficant at higher latitudes and in mountainous environments, where geological and climate factors promote higher rock weathering rates. The enhancement of plant CO<sub>2</sub> uptake via rock nitrogen weathering partially resolves nitrogen-carbon discrepancies in Earth system models and offers an alternative explanation for lack of progressive nitrogen limitation in the terrestrial biosphere. We conclude that natural N inputs impart major control over terrestrial CO<sub>2</sub> sequestration in Earth’s ecosystems.</p>}},
author = {{Dass, Pawlok and Houlton, Benjamin Z. and Wang, Yingping and Wårlind, David and Morford, Scott}},
issn = {{0886-6236}},
keywords = {{bedrock weathering; carbon cycle; nitrogen cycle; nitrogen deposition; nitrogen fixation; nitrogen limitation}},
language = {{eng}},
number = {{10}},
publisher = {{American Geophysical Union (AGU)}},
series = {{Global Biogeochemical Cycles}},
title = {{Bedrock Weathering Controls on Terrestrial Carbon-Nitrogen-Climate Interactions}},
url = {{http://dx.doi.org/10.1029/2020GB006933}},
doi = {{10.1029/2020GB006933}},
volume = {{35}},
year = {{2021}},
}