2006Geophysical Research LettersOpen access

A precisely dated climate record for the last 9 kyr from three high alpine stalagmites, Spannagel Cave, Austria

Nicole Vollweiler, Denis Scholz, Christian Mühlinghaus, Augusto Mangini, Christoph Spötl

Open full text 116 citations

Abstract

Here we use the δ18O time‐series of three stalagmites from the high alpine Spannagel cave (Austria) which grew in small distance from each other to construct a precisely dated, continuous δ18O curve for the last 9 kyr (COMNISPA). This speleothem record is not influenced by effects of kinetic isotope fractionation due to the low temperatures in the cave. Thus, the variations in δ18O can be interpreted in terms of past climate change. COMNISPA exhibits several oscillations within the Holocene, and their timing and duration is in agreement with that documented by other alpine archives.

Open-access reader

About this research paper

What this paper is about

Here we use the δ18O time‐series of three stalagmites from the high alpine Spannagel cave (Austria) which grew in small distance from each other to construct a precisely dated, continuous δ18O curve for the last 9 kyr (COMNISPA). This speleothem record is not influenced by effects of kinetic isotope fractionation due to the low temperatures in the cave. Thus, the variations in δ18O can be interpreted in terms of past climate change. COMNISPA exhibits several oscillations within the Holocene, and their timing and duration is in agreement with that documented by other alpine archives.

Why it matters

OpenAlex reports 116 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Here we use the δ18O time‐series of three stalagmites from the high alpine Spannagel cave (Austria) which grew in small distance from each other to construct a precisely dated, continuous δ18O curve for the last 9 kyr (COMNISPA). This speleothem record is not influenced by effects of kinetic isotope fractionation due to the low temperatures in the cave. Thus, the variations in δ18O can be interpreted in terms of past climate change. COMNISPA exhibits several oscillations within the Holocene, and their timing and duration is in agreement with that documented by other alpine archives.

Key concepts: Stalagmite, Speleothem, Cave, Geology, Holocene, Ice core, δ18O, Climate change

Related papers

Back to paper searchBrowse research topicsOriginal source
A precisely dated climate record for the last 9 kyr from three high alpine stalagmites, Spannagel Cave, Austria — Research Paper | ScholarLens