scholarly journals A flow cytometric method to measure prokaryotic records in ice cores: an example from the West Antarctic Ice Sheet Divide drilling site

2016 ◽  
Vol 62 (234) ◽  
pp. 655-673 ◽  
Author(s):  
PAMELA A. SANTIBÁÑEZ ◽  
JOSEPH R. McCONNELL ◽  
JOHN C. PRISCU

ABSTRACTMicroorganisms were the earliest inhabitants on our planet that occupy nearly every environment, and play a major role in biogeochemical cycles. Despite their global importance, there remains a paucity of data on microbial responses to long-term environmental and climatic changes. Microorganisms are known to be immured in glacial ice, but no high-resolution temporal records of their density exist, owing in large part to the lack of appropriate clean methodology that allows for rapid analysis of samples over depth. We describe a clean and time efficient method that can produce a high-temporal resolution record of prokaryotic density archived in ice cores. The method combines acquisition of discrete samples using a continuous ice-core melting system coupled with flow cytometry (FCM) of DNA-stained samples. Specifically, we evaluate the performance of the FCM measurement technique in terms of specificity, precision, accuracy and minimum detection limits. Examples from the West Antarctic Ice Sheet Divide ice core are included to show the efficacy of the method.

2012 ◽  
Vol 26 (2) ◽  
pp. n/a-n/a ◽  
Author(s):  
Jinho Ahn ◽  
Edward J. Brook ◽  
Logan Mitchell ◽  
Julia Rosen ◽  
Joseph R. McConnell ◽  
...  

2020 ◽  
Author(s):  
Donald Blankenship ◽  
Enrica Quatini ◽  
Duncan Young

<p>A combination of aerogeophysics, seismic observations and direct observation from ice cores and subglacial sampling has revealed at least 21 sites under the West Antarctic Ice sheet consistent with active volcanism (where active is defined as volcanism that has interacted with the current manifestation of the West Antarctic Ice Sheet). Coverage of these datasets is heterogenous, potentially biasing the apparent distribution of these features. Also, the products of volcanic activity under thinner ice characterized by relatively fast flow are more prone to erosion and removal by the ice sheet, and therefore potentially underrepresented. Unsurprisingly, the sites of active subglacial volcanism we have identified often overlap with areas of relatively thick ice and slow ice surface flow, both of which are critical conditions for the preservation of volcanic records. Overall, we find the majority of active subglacial volcanic sites in West Antarctica concentrate strongly along the crustal thickness gradients bounding the central West Antarctic Rift System, complemented by intra-rift sites associated with the Amundsen Sea to Siple Coast lithospheric transition.</p>


2021 ◽  
pp. M55-2019-3
Author(s):  
Enrica Quartini ◽  
Donald D. Blankenship ◽  
Duncan A. Young

AbstractA combination of aerogeophysics, seismic observations and direct observation from ice cores, and subglacial sampling, has revealed at least 21 sites under the West Antarctic Ice Sheet consistent with active volcanism (where active is defined as volcanism that has interacted with the current manifestation of the West Antarctic Ice Sheet). Coverage of these datasets is heterogeneous, potentially biasing the apparent distribution of these features. Also, the products of volcanic activity under thinner ice characterized by relatively fast flow are more prone to erosion and removal by the ice sheet, and therefore potentially under-represented. Unsurprisingly, the sites of active subglacial volcanism that we have identified often overlap with areas of relatively thick ice and slow ice surface flow, both of which are critical conditions for the preservation of volcanic records. Overall, we find the majority of active subglacial volcanic sites in West Antarctica concentrate strongly along the crustal-thickness gradients bounding the central West Antarctic Rift System, complemented by intra-rift sites associated with the Amundsen Sea–Siple Coast lithospheric transition.


2018 ◽  
Vol 48 (4) ◽  
pp. 853-865
Author(s):  
Isaías Ullmann Thoen ◽  
Jefferson Cardia Simões ◽  
Filipe Gaudie Ley Lindau ◽  
Sharon Buchanan Sneed

2014 ◽  
Vol 55 (68) ◽  
pp. 15-26 ◽  
Author(s):  
Joseph M. Souney ◽  
Mark S. Twickler ◽  
Geoffrey M. Hargreaves ◽  
Brian M. Bencivengo ◽  
Matthew J. Kippenhan ◽  
...  

AbstractOn 1 December 2011 the West Antarctic Ice Sheet (WAIS) Divide ice-core project reached its final depth of 3405 m. The WAIS Divide ice core is not only the longest US ice core to date, but is also the highest-quality deep ice core, including ice from the brittle ice zone, that the US has ever recovered. The methods used at WAIS Divide to handle and log the drilled ice, the procedures used to safely retrograde the ice back to the US National Ice Core Laboratory (NICL) and the methods used to process and sample the ice at the NICL are described and discussed.


2017 ◽  
Vol 44 (22) ◽  
pp. 11,482-11,490 ◽  
Author(s):  
Yetang Wang ◽  
Elizabeth R. Thomas ◽  
Shugui Hou ◽  
Baojuan Huai ◽  
Shuangye Wu ◽  
...  

2021 ◽  
Author(s):  
Mackenzie Grieman ◽  
Helene Hoffmann ◽  
Jack Humby ◽  
Robert Mulvaney ◽  
Christoph Nehrbass-Ahles ◽  
...  

<p>The aim of the WArm Climate Stability of the West Antarctic ice sheet in the last INterglacial (WACSWAIN) project is to investigate the possible collapse of the West Antarctic Ice Sheet (WAIS) and its surrounding ice shelves during the Last Interglacial (~120,000 years ago).  As part of this project, a 651-meter ice core was drilled to bedrock at Skytrain Ice Rise in Antarctica during the 2018/2019 field season.  Ions and elements originating from marine sources along with water isotope content in this ice core can be used to infer changes in ice sheet and ice shelf extent.  The stable water isotope signal has the potential to capture both regional climate change and changes in the elevation of the drilling site through time.  Marine chemical content in the ice core could indicate variability in the proximity of the site to a marine environment.  Water isotopes and chemical impurities in the ice core were analysed continuously using cavity ring down spectroscopy and inductively coupled plasma mass spectrometry, respectively. As expected, δ<sup>18</sup>O and δD increase from the last glacial maximum to the Holocene.  δ<sup>18</sup>O and δD increase and sodium and magnesium levels decline from deglaciation into the early Holocene. δ<sup>18</sup>O and δD show an abrupt increase in the early Holocene at about 8,000 years before present.  Sea salt similarly increases 2-fold and becomes more variable about 1,000 years later (7,000 years before present).  These increases could indicate a retreat of the ice shelf to its current position.</p>


2016 ◽  
Vol 121 (5) ◽  
pp. 907-924 ◽  
Author(s):  
Michelle R. Koutnik ◽  
T. J. Fudge ◽  
Howard Conway ◽  
Edwin D. Waddington ◽  
Thomas A. Neumann ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document