The stable carbon isotope composition of bulk organic matter is affected by changes in the terrestrial contribution to the total organic carbon (TOC) (Kuypers et al., 2004): Cretaceous marine organic matter typically yields δ 13 C values that are lower by 3 to 4‰ compared to coeval land plant or terrestrial organic C, so changing ratios of ...
The mechanisms by which lime and/or phosphate addition impacts the preservation of soil organic matter (OM) are poorly understood. We explored the changes in quantity and chemistry of water-extractable organic matter (WEOM) in the bulk soil and its heavy density fraction (>1.6 g/cm 3) of an unmanaged C-rich volcanic soil caused by …
In high N and low C sediments, studies have often found that the availability of organic carbon becomes a limiting factor for denitrification processes (Grebliunas and Perry, 2016). For headwater river ecosystems, the confluence of surface or subsurface runoff into rivers is often accompanied by higher terrestrial C source inputs and lower N ...
We determined soil organic carbon (SOC) accumulation rates and stability in the initially C-free model soils. Across all model soils, SOC increased consistently over time (P<0.05; Table 1).
The cycle of organic carbon through the atmosphere, oceans, continents and mantle reservoirs is a hallmark of Earth. Over geological time, chemical exchanges between those reservoirs have...
INTRODUCTION. Recycling of organic matter in sediments is an important component of biogeochemical cycles because marine sediments are critical for long-term carbon storage (1, 2).Prokaryotes in deep oceanic subsurface account for more than 25% of global cell numbers (), and it is still controversial whether Archaea or Bacteria are …
Despite considerable research, predicting how soil organic carbon (SOC) in grain production systems will respond to conservation management practices, such as reduced tillage, residue retention and alternative rotations, remains difficult because of the slowness of change and apparent site specificity of the effects. We compared SOC …
For example, vegetation restoration can improve soil organic carbon storage, soil aggregate stability, and soil and water conservation (Liu et al., 2019). Returning farmland to forest can increase organic carbon storage by 20–50%, but converting forest to farmland can reduce organic carbon storage by ∼ 40% (Guo and Gifford, 2002).
14 C provides a useful tracer of carbon sources in many surficial environments. Atmospheric CO 2 is enriched in 14 C, which decays to 14 N with a half-life of 5730 years. Thus, any organic material greater than ∼60,000 years in age, or any biomolecule assembled from an ancient carbon source, contains essentially no 14 C. …
Forest thinning is a common forest management practice and has complex effects on soil organic carbon (SOC). However, the mechanisms underlying SOC and its components (physical fractions and chemical compositions) in response to forest thinning remain poorly understood. Four thinning treatments including control (CK with no thinning), light …
The Woodford Shale core recovery is 41 m thick in the Wyche core, 11 m thick in the East Fitts core and 15 m thick in the Chitwood–Harris core (Fig. 1), and is primarily composed of organic rich shale (Fig. 2 f) with intermittent chert intervals (1–10 cm thick) as well as more silty intervals.All sediments lack evidence of storm-wave reworking …
Understanding the soil organic matter (SOM) dynamics in forest ecosystems is important because soils are the largest pool of carbon (C) on Earth [6,7].As a key ecological process responsible for the transfer of organic matter from vegetation to soil, plant litter decomposition plays a critical role in global C cycling [8,9,10].Plant …
Extremely low δ¹³C values of total inorganic carbon and organic carbon, increased Methane Index, and molybdenum (Mo) and uranium (U) enrichments at depths of 225–255 cm below the sea-floor ...
Request PDF | Heavy thinning reduces soil organic carbon: Evidence from a 9-year thinning experiment in a pine plantation | Forest thinning is a common forest management practice and has complex ...
Soils store more carbon (C) belowground than plants and the atmosphere combined, providing a critical ecosystem service. While previous research has shown that sustainable forest management practices can increase soil C storage by enhancing plant productivity, the role of soil microbes remains elusive. We analyzed changes in plant …
The soil organic carbon stocks were calculated using the following equations (Deng et al., 2016): (4) S O C S t o c k = S O C × B D × T 10 where SOC Stock represents soil organic carbon stocks (Mg∙ha −1), SOC represents the soil organic carbon content (g∙kg −1), BD represents the soil bulk density (g∙cm −3), and T …
Biochar is a carbon-rich material that increases soil C sequestration and mitigates climate change. However, due to the variability of experimental conditions, types of biochar and soil, the influence of biochar on the accumulation of different soil carbon fractions remains unclear. Therefore, a meta-analysis was performed that included 586 ...
Here, we present analyses of multiple high-resolution TOC and stable organic carbon isotope (δ 13 C org) records from the middle to high latitudes during the past 100 Ma ( …
1. Introduction. Globally, soil contains 1500–2300 Pg of organic carbon (OC), approximately twice as much as the amount in the atmosphere and three times the amount in terrestrial vegetation (Lal, 2004), and thus has a most important role in balancing atmospheric carbon dioxide (CO 2) concentration (Briones et al., 2006).Whether soil …
Our study. δ. provides the petrological evidence for the subduction of surface-derived organic carbon to the mantle depths of approximately 90 km, with the formation of graphitized organic carbon ...
Abstract. The increasing concentration of CO 2 in the atmosphere is perturbing the global carbon (C) cycle, altering stocks of organic C, including soil …
PDF | On May 1, 2023, Yongxue Yan and others published Wollastonite addition stimulates soil organic carbon mineralization: Evidences from 12 land-use types in subtropical China | Find, read and ...
The SOC pool comprises approximately 2/3 of the terrestrial organic carbon (Post et al., 1990; Amundson, 2001). Its alteration in response to N enrichment may significantly influence the carbon dioxide (CO 2 ) concentration in atmosphere and thus has implications for global C cycle and climate change.
Soil organic carbon (SOC) turnover is a key parameter in the terrestrial ecosystem model and ecosystem management (Tan et al., 2020), and SOC pool is the largest terrestrial C reservoir (Amundson, 2001). Thus, the changes in SOC turnover caused by decreased N deposition might significantly affect global C cycle and further …
Sulfate-driven anaerobic oxidation of methane (AOM) limits the release of methane from marine sediments and promotes the formation of carbonates close to the seafloor in seepage areas along continental margins. It has been established that hydrocarbon seeps are a source of methane, dissolved inorganic carbon, and dissolved …
Soil erosion has a significant impact on the distribution and sequestration of soil carbon, affecting the global C cycle. Although the transport and transformation of soil organic carbon (SOC) during the erosion process have been widely studied, there is still a lack of understanding of the impacts of soil erosion on soil inorganic carbon (SIC) and its …
Wollastonite addition stimulates soil organic carbon mineralization: Evidences from 12 land-use types in subtropical China - ScienceDirect. CATENA. …
However, direct evidence of high organic carbon export fluxes to the early Cambrian seafloor is lacking, so a key test of the "organic carbon burial hypothesis" for the Cambrian Explosion has not been undertaken to date. Both Mo (δ 98 Mo) and U isotopes (δ 238 U) in organic-rich black shales have been used to track local and global …
The top two metres of soils store more than 2,200–2,500 Pg of organic carbon (C) 1,2, representing the largest biologically active C pool in terrestrial ecosystems 3.The size of this C reservoir ...
The transport of dissolved organic carbon from land to ocean is a large dynamic component of the global carbon cycle. Inland waters are hotspots for organic matter turnover, via both biological ...