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Water content and Loss on ignition determination of Late Quaternary sediments...
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Loss on ignition of sediment core IZN_19-31 from Lake Iznik (NW Turkey)
The loss on ignition (LOI) analysis was performed in 2019 on the IZN19_31 Sequence, with a 10-cm sampling interval all along the sequence to estimate organic matter (OM) and... -
Loss on ignition of sediment core IZN19-24 from Lake Iznik (NW Turkey)
The LOI method allows us to estimate the organic matter and carbonate content of lake sediments. LOI analysis was performed on the IZN19-15 and IZN19-24 cores with a 10-cm... -
Loss on ignition of sediment core IZN19-15 from Lake Iznik (NW Turkey)
The LOI method allows us to estimate the organic matter and carbonate content of lake sediments. LOI analysis was performed on the IZN19-15 and IZN19-24 cores with a 10-cm... -
Minerogenic content as a storminess proxy from Cors Fochno, Wales
A 4 m long peat core was sampled using a Russian corer from the centre of the bog (52°30'9''N; 4°0'39''W). Chronological constraints were provided by AMS radiocarbon dating of 5... -
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain
Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and... -
Sand-based storminess proxies from a coastal peatland Hill Top Bog, Outer Heb...
Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this... -
Sand-based storminess proxies from a coastal peatland Struban Bog, Outer Hebr...
Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this...