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δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
This dataset has no description
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Mg/Ca and different methods to calculate SST at ODP Sites 165-999 and 144-871
This dataset has no description
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Isotopes measured on Uvigerina peregrina, Globigerinoides ruber sensu stricto...
This dataset has no description
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Isotopes measured on Cibicidoides wuellerstorfi from ODP Site 165-999
This dataset has no description
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δ¹¹B-derived pCO₂ calculated with different treatments of Mg/Ca-derived SST a...
pCO₂ (in parts per million) calculated from δ¹¹B as the maximum probability of 10,000 realisations of the Monte Carlo simulation, and calculated with different Mg/Ca-temperature... -
Fragmentation index and percentage sand from ODP Site 144-871
This dataset has no description
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High resolution incubation measurements
Soil samples were taken in the bog site of the Siikaneva peat complex and adjacent shrub-belt and forest site in Ruovesi, Finland. Samples were characterized by measuring water... -
Anaerobic incubation measurements (CH4+CO2) from samples of Lena Delta collec...
The data sets were made during the summer 2021, with samples collected from three cores, at two depths (active and permafrost layers). In total, six samples (3 replicates by... -
Splines of reconstructed deep ocean 14C ages over that last 25 kyr and simula...
Carbon cycle models used to interpret the IntCal20 compilation of atmospheric ∆14C have so far neglected a key aspect of the millennial-scale variability connected with the... -
Anaerobic respiration in a boreal wetland and surrounding habitats, across a ...
This dataset reports measurements from a laboratory incubation of soils sourced from a boreal peatland and surrounding habitats (Siikaneva Bog, Finland). In August 2021, soil... -
Salinity, depth, current, temperature, dissolved oxygen, carbon dioxide, rado...
Salinity, depth, current, temperature, oxygen, carbon dioxide (CO2), radon (222Rn), pH and chlorophyll hourly variation during a complete neap to spring tidal cycle in 2... -
Physical oceanography and CO2 measurements from Develogic Modular Seafloor La...
The Modular Seafloor Lander (MSL) is a submersible autonomous device manufactured by Develogic GmbH subsea systems. The MSL was deployed at 15:18h on 22 July 2022 and recovered... -
A regional pCO2 climatology of the Baltic Sea
Based on direct surface pCO2 observation and a model-based extrapolation technique, we established a regional pCO2 climatology of the Baltic Sea. Observations from June 2003 to... -
CO2 Vertical Profiles on Four Sites over Amazon from 2019 to 2020
To improve diagnosis of Amazonia's carbon cycle, we present a 2 year data (2019 to 2020), complementary to our previosly 9 years (2010 to 2018) observations of lower troposphere... -
OceanSODA-UNEXE: Gridded surface ocean carbonate system datasets in the Amazo...
Within the European Space Agency funded Oceanographic datasets for acidification (OceanSODA) project, the University of Exeter (UNEXE) produced the OceanSODA-UNEXE dataset... -
Climatic simulation from the equatorial Indian Ocean
During the late Miocene, global cooling occurred alongside the establishment of near-modern terrestrial and marine ecosystems. Significant (3 to 5 °C) sea surface cooling from... -
Plio-Pleistocene simulations from a global carbon cycle box model
Atmospheric CO2 reconstructions beyond ice core records are based on geochemical proxies, which bear proxy-specific intrinsic uncertainties. Here, we use the global carbon cycle... -
Cenozoic CO2 from marine proxies
Atmospheric CO2 has been reconstructed over the last 66 million years from two marine proxies: the boron isotope composition of foraminifera and the carbon isotope composition... -
KOSMOS 2017 Peru mesocosm study: carbonate chemistry data
Oxygen minimum zones (OMZs) in the ocean are characterized by enhanced carbon dioxide (CO2) levels and are being further acidified by increasing anthropogenic atmospheric CO2.... -
Simulation results for the role of the deglacial buildup of the Great Barrier...
The carbon isotope 13C is commonly used to attribute the rise of atmospheric CO2 during the last deglaciation to various processes. Here we discuss the role of the growth of the...