Effect of Global Change on the Primary Production of Antarctic coastal Ecosystems
Entry ID:
ASAC_2518
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Summary
Abstract:
Metadata record for data from ASAC Project 2518 See the link below for public details on this project. Global climate change will lead to a reduction in the duration and thickness of sea ice in coastal areas. We will determine whether this will lead to a decrease in primary production and food value to higher predators. Project objectives: Our primary objective is to determine what effect will ... declining sea ice cover have on Antarctic coastal primary production?
Hypotheses to be tested
- A decrease in sea ice algal production will lead to a net reduction in total primary production.
- A decrease in sea ice will result in less water column stratification which will reduce the significance of phytoplankton blooms.
- Less sea ice will lead to a change in phytoplankton bloom composition away from diatoms towards un-nutritious nuisance blooms such as Phaeocystis
- Benthic microalgal production will increase
- Seaweed production will increase slightly
- A decrease in sea ice thickness will increase ice algal production (as they are generally light limited)
- Ice algae, benthic microalgae, and phytoplankton will acclimate to an elevated light climates by changing their photosynthetic efficiency and capacity
- Ice algae, benthic microalgae, and phytoplankton will acclimate to an altered light quality.
To answer these questions we will also need to determine:
- What is the total annual primary production at coastal Antarctic sites; this consists of the contributions from the sea ice algal mats, benthic microalgal, seaweed and phytoplankton?
- What is the effect of major environmental variables, such as UV, salinity, currents oxygen toxicity, cloud cover, nutrient availability and temperature on production.
- What is the inter-annual variability in primary production?
A broader scale issue that our data will contribute to providing answers to is the question
- What effect will changing primary production have on higher trophic levels?
Taken from the 2009-2010 Progress Report:
Progress against objectives:
The 2009/10 field and laboratory season focused on the second of our primary questions, i.e. 'What is the effect of major environmental variables, such as UV, salinity, currents oxygen toxicity, cloud cover, nutrient availability and temperature on production'. In particular we focused on light and light transmission though the sea ice.
The science program AAS2518 was executed at Casey station from 11 Nov to 5 Dec 2009. The project was split into a field and a lab-based component. In situ spectral light transmission data were collected on first year sea ice within the vicinity of Jack's Hut. Ice cores were collected and transported to the laboratory at Casey station for spectral attenuation profiles within sea ice, and for measurements of spectral absorption by particulate and dissolved organic matter.
Overall, the program was successful: in situ sea-ice spectral transmission data was collected in combination with vertical profiles of absorption coefficients of particulate (algae and detritus) and dissolved organic matter. Samples for analysis of photosynthetic pigments were collected and shipped to Sydney. Their analysis is underway. Due to logistical issues associated with the collection and transport of sea ice cores, the protocol for vertical profiling of spectral attenuation was modified (see below) and analysis of the data is currently underway.
The field component of the program was successful as spectral transmission data was collected for first year sea-ice, and the chosen site contained a thriving sea ice algal community for bio-optical measurements. It was initially planned to sample multiple sites offering a range of varying sea-ice thickness, but this was not possible during this campaign. Many sites in the vicinity of Casey station had already started to melt and break up, so that for logistical and safety reasons the area around Jack's hut was the only workable option. The field period instead spanned ~ 20 days during the melt period at Jack's, during which the porosity of sea ice increased but thickness remained constant.
Ice cores destined for spectral transmission profiles were to be collected whole and intact, but due to the presence of fractures in the sea ice, drilling (manual as well as motor powered) resulted in fractured core samples. The protocol was therefore modified: cores were sectioned in 20 cm sections and spectral transmission measured for each section. Spectral transmission profiles across the entire thickness of sea ice are to be re-constructed from the discrete data points. The accuracy of the approach will be assessed against the in situ spectral transmission data.
The download file contains three spreadsheets (two of them are csv files), and a readme document which provides detailed information about the three spreadsheets. 
Related URL
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Description:
Data download page.
Description:
Maps in PDF and PNG formats.
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Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
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N: 90.0
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S: -90.0
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E: 180.0
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W: -180.0
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Data Set Citation
Dataset Originator/Creator:
Wildlife Conservation Society (WCS), and Center for International Earth Science Information Network (CIESIN)/Columbia University
Dataset Title:
Last of the Wild Project, Version 2, 2005 (LWP-2): Global Human Influence Index (HII) Dataset (Geographic)
Dataset Release Date:
2005
Dataset Release Place:
Palisades, NY
Dataset Publisher:
NASA Socioeconomic Data and Applications Center (SEDAC)
Version:
2.00
Data Presentation Form:
raster, map
Online Resource:
http://sedac.ciesin.columbia.edu/data/set/wildareas-v2-human-influe...
Temporal Coverage
Start Date:
1995-01-01
Stop Date:
2004-01-01
Quality
Species identification accurate, assessment of species rarity is done with
local species experts and is as accurate as possible given the current state of
species information.Occurrence location data for populations of rare species of
anadromous fish and marine birds are included for a jurisdiction (an Atlantic
province plus Labrador) only if the species is determined to be rare in that
jurisdiction. Data for occurrences of rare species of marine mammals is
included for the Bay of Fundy only.
Data are usually requested by species or by location (e.g., at a given locale
or within a specified area, the identification of all rare species present)
Access Constraints
none
Use Constraints
noneData users are advised that ACCDC data does not provide a conclusive
statement on the presence, absence or condition of rare species in any part of
Atlantic Canada. The ACCDC makes a strong effort to verify the accuracy of all
the data it obtains, generates and manages, but it will not be held responsible
for inaccuracies in data that it provides. Data accuracy is qualified as to
the date of the survey from which the AC CDC compiled the rare species data
into its databases.
Data Set Progress
IN WORK
Data Center
Atlantic Canada Conservation Data Centre
Data Center URL:
http://www.accdc.com/
| Data Center Personnel |
Name:
R.
A.
LAUGENSCHLAGER
Phone:
(506) 364-2661
Email:
rlautenschlager at mta.ca
Contact Address:
Atlantic Canada Conservation Data Centre
P.O. Box 6416
City:
Sackville
Province or State:
New Brunswick
Postal Code:
E4L 1G6
Country:
Canada
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| Data Center Personnel |
Name:
KATE
BREDIN
Phone:
+01-506-364-2660
Fax:
+01-506-364-2656
Email:
kbredin at mta.ca
Contact Address:
P.O. Box 6416
City:
Sackville
Province or State:
New Brunswick
Postal Code:
E4L 1G6
Country:
Canada
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Personnel
Role:
DIF AUTHOR
Phone:
+01-506-364-2660
Fax:
+01-506-364-2656
Email:
kbredin at mta.ca
City:
Sackville
Province or State:
New Brunswick
Postal Code:
E4L 1G6
Country:
Canada
Role:
TECHNICAL CONTACT
Phone:
(506) 364-2661
Email:
rlautenschlager at mta.ca
Contact Address:
Atlantic Canada Conservation Data Centre
P.O. Box 6416
City:
Sackville
Province or State:
New Brunswick
Postal Code:
E4L 1G6
Country:
Canada
Creation and Review Dates
DIF Creation Date:
2004-03-02
Last DIF Revision Date:
2005-12-05
Future DIF Review Date:
2005-01-16
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