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MICADAS C dating facility. First year of routine measurements at the AWI

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Torben Gentz1, Elizabeth Bonk1, Jens Hefter1, Hendrik Grotheer1, Gesine Mollenhauer1,2,3

BREMERHAVEN

Am Handelshafen 12 27570 Bremerhaven Telefon 0471 4831-0 www.awi.de

The main goal for the facility at AWI is the precise and independent dating of carbonaceous materials in marine and terrestrial sediments, sea-ice, and water. A wide range of in-house research topics address various processes of global carbon cycling. A particular focus is on sediments from high latitude oceans, in which radiocarbon-based age models are often difficult to obtain due to the scarcity of carbonate microfossils or organic matter. The wide range of applications encompass gas analyses of small-sized samples of foraminifera, specific (biomarker) compounds and other organics as well as analyses of graphite targets containing ~1mg to 250µg carbon. This requires establishing routine protocols of various sample preparation techniques utilizing state of the art peripheral prepping systems. In this context, it is important to know if the results of different sample introduction techniques are comparable to each other and to international standards.

Introduction

In November 2016, the first Mini-Carbon-Dating-System (MICADAS) manufactured by Ionplus AG was delivered and installed at the Alfred-Wegener-Institute (AWI), Germany.

Results

First year of routine measurements at the AWI MICADAS 14 C dating facility.

1. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, 25570 Bremerhaven, Germany 2. Department of Geosciences, University of Bremen, 28359 Bremen, Germany

3. MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany

Gas Graphite

C7-Oxalic acid

C5-Wood

Gas Graphite

Average

Gas Graphite

Coral

Graphite C2-Travertine

Gas

A comparison of gas (EA/CHS-GIS) or graphite (EA/CHS-AGE) measurements was performed on organic and inorganic material with varying F14C values between 0.22 – 0.95. International standard materials (IAEA) as well as a carbonate (established as internal standard by Ellen Druffel at the University of California, Irvine) were used. Gas samples were analyzed at a standard size of ~100 µgC, graphite samples ~ 1000 µgC. A conservative target scatter of 0.5 % was calculated for graphite samples and 1 % to 1.5 % for gas samples.

Fig. 1 Fig. 2

Nominal value

Legend

Gas samples

Graphite samples

If you have further questions or remarks please contact us:

Torben.Gentz@awi.de

Gesine.Mollenhauer@awi.de Micadas@awi.de or

www.awi.de/en/science/geosciences/marine-geochemistry/micadas.html

Conclusions

 The results show a comparison in between the errors amoung both introduction techniques and reference material.

 The target scatter can be lowered significantly for future measurements.

 In the first year of routine operation we established several analysis techniques with different pre-instruments with special focus on forams and specific compounds (biomarkers).

Further information can be seen on the poster „Low blank compound specific radiocarbon analysis at the AWI-MICADAS facility“ (Session G1; Nr. 38).

Routine operations at AWI-Facilities

established In progress planned

Average

Gas Graphite

Literature Gas Graphite

Literature

Fig. 1.: F14C values of organic material (IAEA C5 and IAEA C7) as gas or graphite measurements .

Fig. 2.: F14C values of anorganic material (IAEA C2 and internal coral standard) as gas or graphite measurements.

Tab. 1.: F14C values of organic material. C5 and C7 are shown in Fig. 1. Messelshale and Kuhgraben are internal standards.

Organics Material measured value [F14C] ± n measured value [F14C] ± n reference value [F14C] ±

IAEA-C5 wood 0.2300 0.0039 13 0.2303 0.0013 9 0.2305 0.0002

IAEA-C7 oxalic acid 2 0.4939 0.0038 10 0.4958 0.0017 18 0.4953 0.0012

Messel Shale blank sediment -0.0063 0.0032 10 0.0006 0.0014 29 no

Kuhgraben modern sediment 0.8468 0.0102 10 0.8563 0.0121 12 no

EA-AGE EA-GIS

Carbonates Material measured value [F14C] ± n measured value [F14C] ± n reference value [F14C] ±

IAEA-C1 marble 0.0001 0.0007 10 0.0013 0.00058 12 0 0.0002

IAEA-C2 travertine 0.4098 0.0041 10 0.4116 0.0023 15 0.4114 0.0003

Blank Forams foraminifera 0.0049 0.0011 140 0.0025 0.0004 9 no

CAHI coral coral 0.9391 0.0059 9 0.9412 0.0049 11 0.9444 0.0018

CHS-GIS CHS-AGE

Tab. 2.: F14C values of anorganic material. C2 and CAHI coral (internal standard by Ellen Druffel) are shown in Fig. 2.

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