Glacial/interglacial variations in methanesulfonate (MSA) in the Siple Dome ice core, West Antarctica

[1] Methanesulfonate (MSA) in the Siple Dome ice core is a record of the deposition of biogenic sulfur to the West Antarctic ice sheet covering the past 100 kyr. Siple Dome MSA levels were low during the last glacial maximum, and increased to higher Holocene levels with a several kyr lag relative to...

Full description

Bibliographic Details
Main Authors: Eric S. Saltzman, Irina Dioumaeva, On D. Finley, I. Dioumaeva, B. D. Finley
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
variations in methanesulfonate (MSA) in the Siple Dome ice core
Antarctic
East Antarctica
Greenland
Pacific
Renland
Siple
Siple Dome
Southern Ocean
West Antarctic Ice Sheet
West Antarctica
Antarc*
Antarctica
Greenland ice cores
GRIP
ice core
Ice Sheet
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.503.3703
http://www.ess.uci.edu/~esaltzma/pub_pdfs/SaltzmanetalGRL06.pdf
Description
Summary:[1] Methanesulfonate (MSA) in the Siple Dome ice core is a record of the deposition of biogenic sulfur to the West Antarctic ice sheet covering the past 100 kyr. Siple Dome MSA levels were low during the last glacial maximum, and increased to higher Holocene levels with a several kyr lag relative to the deglacial warming. The positive correlation between MSA and temperature at Siple Dome is similar to that in Greenland ice cores (Renland, GISP2, and GRIP), and stands in contrast to the negative correlation observed at Vostok, East Antarctica. The Siple Dome MSA data suggest that the sign of the high latitude dust/sulfur/climate feedback is negative, at least for the Pacific sector of the high latitude Southern ocean. These results challenge the idea that fertilization by increased dust deposition led to widespread increased DMS emissions from this region of

Similar Items