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Aeolian sediment in snow and on sea ice in Western in McMurdo Sound, and the Nansen Ice Shlelf in Terra Nova Bay, Antarctica

Entry ID: K001D_2010_2012_NZ_1

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Summary

Abstract: To quantify the distribution, composition and overall flux of aeolian (windblown) sediment that accumulates on Ice shelves and annual sea ice in the SW Ross Sea region and is subsequently released into the water column during melting. The sediment is an important contributor to sea floor sedimentation and is thought to be an important source of the micro-nutrient iron (Fe), triggering vast ... phytoplankton blooms each spring in the Ross Sea Region. These blooms are major productivity events that contribute large volumes of biogenic sediment to the seafloor and ultimately to the stratigraphic record (e.g. ANDRILL cores). Although the contribution of aeolian sediment has long been considered important, the actual flux of such material, its Fe content and availability to phytoplankton is poorly known. Understanding these modern processes is a key part of interpreting the past record of environmental change in the region.

Field work carried out in the 2010/11 season retrieved a network of samples from the surface of the sea ice in Western McMurdo Sound and covers almost all previous geological drill sites (CRP1,2,3; CIROS 1,2; ANDRILL- 2a). 500ml bottles of snow were collected with trace metal clean technique and bags of snow (and dust) from a grid of sites (2.5 and 5km spacing) on the Western side of McMurdo Sound. This unprecedented dataset will for the first time allow us to quantify the flux, size range and provenance of aeolian sediment entering the McMurdo Sound and evaluate its importance as both a direct sediment contributor and also as a source of Fe influencing the regional biogeochemical cycle.

Fieldwork carried out in the 2011/12 season strengthened this dataset by resampling keys sites from the 2010/11 survey in Southern McMurdo Sound to investigate inter-annual variability. In addition, a firn core was collected from Windless Bight at the same location as a core recovered in 2006 (Dunbar et al. 2009). Preliminary analysis on this core has shown clear annual layering and promising potential for extracting a record of dust to overlapping with previous cores (Atkins et al. 2011.) The sampling for the season involved collecting bags of snow from sea ice and ice shelf surfaces, short firn cores (up to 5m), aeolian sediment trap samples, geological samples and climate station data (wind speed and dirtection) in Southern McMurdo Sound and Nansen Ice shelf, Terra Nova Bay, Antarctica to quantify aeolian sediment distribution.

The main focus of the 2011/12 season was in the Terra Nova Bay area. This region has a well-studied polnyna and annual algal bloom. In addition it is renowned for its katabatic airflow. A major limitation for understanding the biogeochemical cycles in the area is the lack of quantitative data on aeolian dust flux. Custom-built sediment traps and a climate station were deployed along the edge of the Nansen Ice Shelf during November to January. In addition, surface snow samples, short firn cores and exposed rocks were sampled in the region to help quantify the dust flux into the Terra Nova Bay polnyna. Preliminary analysis shows that the sediment traps were an effective way of sampling aeolian sediment and dust from snow samples has allowed us to begin mapping the sediment distribution and transport pathways at Terra Nova Bay.

Related URL

Link: VIEW PROJECT HOME PAGE

Geographic Coverage

(Click for Interactive Map)

Spatial coordinates

	N: -76.82	S: -77.77	E: 163.0	W: 165.91
Min Altitude: 0 Max Altitude: 0
Min Depth: 0 Max Depth: 0

	N: -76.67	S: -77.0	E: 165.91	W: 162.4
Min Altitude: 0 Max Altitude: 0
Min Depth: 0 Max Depth: 0

	N: -74.46	S: -77.89	E: 163.5	W: 167.08
Min Altitude: 0 Max Altitude: 393
Min Depth: 0 Max Depth: 5.25

	N: -74.84	S: -77.89	E: 167.08	W: 163.5
Min Altitude: 0 Max Altitude: 393
Min Depth: 0 Max Depth: 5.25

Parent DIF

This data set description is a member of a collection. The collection is described in
K001_ANDRILL

Temporal Coverage

Start Date: 2010-10-26

Stop Date: 2010-11-25

Start Date: 2011-11-22

Stop Date: 2011-12-25

Location Keywords

CONTINENT > ANTARCTICA

CONTINENT > ANTARCTICA > McMURDO SOUND

GEOGRAPHIC REGION > POLAR

CONTINENT > ANTARCTICA > TERRA NOVA BAY

Science Keywords

BIOSPHERE > AQUATIC ECOSYSTEMS

BIOSPHERE > AQUATIC ECOSYSTEMS > PLANKTON

ISO Topic Category

CLIMATOLOGY/METEOROLOGY/ATMOSPHERE

GEOSCIENTIFIC INFORMATION

Platform

FIELD INVESTIGATION

Instrument

GPS > Global Positioning System

Project

ANDRILL > Antarctic Drilling Program

Quality All samples and data are stored Victoria University of Wellington and GNS Science.
If you require any further information please contact Cliff Atkins.

Data Set Progress

IN WORK

Data Center

Antarctica New Zealand, New Zealand Antarctic Institute, New Zealand

Data Center URL: http://www.antarcticanz.govt.nz/

Data Center Personnel
Name: CAROLINE MACLAURIN Phone: (03) 358 0200 Fax: (03) 358 0211 Email: c.maclaurin at antarcticanz.govt.nz Contact Address: Antarctica New Zealand Private Bag 4745 City: Christchurch 8140 Country: New Zealand

Personnel

CLIFF ATKINS

Role: INVESTIGATOR

Phone: +64 4 463 6143

Fax: +64 4 463 5186

Email: cliff.atkins at vuw.ac.nz

Contact Address:

School of Geography, Environment and Earth Sciences

Victoria University of Wellington

PO BOX 600

City: Wellington

Country: New Zealand

TIM NAISH

Role: INVESTIGATOR

Phone: +64 4 463 6197

Fax: +64 4 463 5186

Email: tim.naish at vuw.ac.nz

Contact Address:

Antarctic Research Unit

Victoria University of Wellington

PO BOX 600

City: Wellington

Postal Code: 6140

Country: New Zealand

Publications/References

Atkins, C.B., 2011 ‘The answer is blowing in the wind’. Antarctic, The publication of the New Zealand Antarctic Society, Vol 29, No.1, Issue 215, pp.22-23

Creation and Review Dates

DIF Creation Date: 2012-05-29

Last DIF Revision Date: 2012-06-15

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