Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake

Lake Vanda is a perennially ice-covered, closed-basin lake in the McMurdo Dry Valleys, Antarctica. Laminated photosynthetic microbial mats cover the floor of the lake from below the ice cover to >40 m depth. In recent decades, the water level of Lake Vanda has been rising, creating a “natural exp...

Full description

Bibliographic Details
Published in:Biology
Main Authors: Ian Hawes, Dawn Sumner, Dale Andersen, Anne Jungblut, Tyler Mackey
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2013
Subjects:
Online Access:https://doi.org/10.3390/biology2010151
id ftmdpi:oai:mdpi.com:/2079-7737/2/1/151/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2079-7737/2/1/151/ 2023-08-20T04:01:02+02:00 Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake Ian Hawes Dawn Sumner Dale Andersen Anne Jungblut Tyler Mackey agris 2013-01-25 application/pdf https://doi.org/10.3390/biology2010151 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/biology2010151 https://creativecommons.org/licenses/by/3.0/ Biology; Volume 2; Issue 1; Pages: 151-176 cyanobacteria benthic communities microbial mat environmental change Antarctic lake Text 2013 ftmdpi https://doi.org/10.3390/biology2010151 2023-07-31T20:31:24Z Lake Vanda is a perennially ice-covered, closed-basin lake in the McMurdo Dry Valleys, Antarctica. Laminated photosynthetic microbial mats cover the floor of the lake from below the ice cover to >40 m depth. In recent decades, the water level of Lake Vanda has been rising, creating a “natural experiment” on development of mat communities on newly flooded substrates and the response of deeper mats to declining irradiance. Mats in recently flooded depths accumulate one lamina (~0.3 mm) per year and accrue ~0.18 µg chlorophyll-a cm−2 y−1. As they increase in thickness, vertical zonation becomes evident, with the upper 2-4 laminae forming an orange-brown zone, rich in myxoxanthophyll and dominated by intertwined Leptolyngbya trichomes. Below this, up to six phycobilin-rich green/pink-pigmented laminae form a subsurface zone, inhabited by Leptolyngbya, Oscillatoria and Phormidium morphotypes. Laminae continued to increase in thickness for several years after burial, and PAM fluorometry indicated photosynthetic potential in all pigmented laminae. At depths that have been submerged for >40 years, mats showed similar internal zonation and formed complex pinnacle structures that were only beginning to appear in shallower mats. Chlorophyll-a did not change over time and these mats appear to represent resource-limited “climax” communities. Acclimation of microbial mats to changing environmental conditions is a slow process, and our data show how legacy effects of past change persist into the modern community structure. Text Antarc* Antarctic Antarctica McMurdo Dry Valleys MDPI Open Access Publishing Antarctic Basin Lake ENVELOPE(161.917,161.917,-76.150,-76.150) Lake Vanda ENVELOPE(161.600,161.600,-77.517,-77.517) McMurdo Dry Valleys Pinnacle ENVELOPE(-54.900,-54.900,-61.067,-61.067) Vanda ENVELOPE(161.550,161.550,-77.533,-77.533) Biology 2 1 151 176
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic cyanobacteria
benthic communities
microbial mat
environmental change
Antarctic lake
spellingShingle cyanobacteria
benthic communities
microbial mat
environmental change
Antarctic lake
Ian Hawes
Dawn Sumner
Dale Andersen
Anne Jungblut
Tyler Mackey
Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
topic_facet cyanobacteria
benthic communities
microbial mat
environmental change
Antarctic lake
description Lake Vanda is a perennially ice-covered, closed-basin lake in the McMurdo Dry Valleys, Antarctica. Laminated photosynthetic microbial mats cover the floor of the lake from below the ice cover to >40 m depth. In recent decades, the water level of Lake Vanda has been rising, creating a “natural experiment” on development of mat communities on newly flooded substrates and the response of deeper mats to declining irradiance. Mats in recently flooded depths accumulate one lamina (~0.3 mm) per year and accrue ~0.18 µg chlorophyll-a cm−2 y−1. As they increase in thickness, vertical zonation becomes evident, with the upper 2-4 laminae forming an orange-brown zone, rich in myxoxanthophyll and dominated by intertwined Leptolyngbya trichomes. Below this, up to six phycobilin-rich green/pink-pigmented laminae form a subsurface zone, inhabited by Leptolyngbya, Oscillatoria and Phormidium morphotypes. Laminae continued to increase in thickness for several years after burial, and PAM fluorometry indicated photosynthetic potential in all pigmented laminae. At depths that have been submerged for >40 years, mats showed similar internal zonation and formed complex pinnacle structures that were only beginning to appear in shallower mats. Chlorophyll-a did not change over time and these mats appear to represent resource-limited “climax” communities. Acclimation of microbial mats to changing environmental conditions is a slow process, and our data show how legacy effects of past change persist into the modern community structure.
format Text
author Ian Hawes
Dawn Sumner
Dale Andersen
Anne Jungblut
Tyler Mackey
author_facet Ian Hawes
Dawn Sumner
Dale Andersen
Anne Jungblut
Tyler Mackey
author_sort Ian Hawes
title Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
title_short Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
title_full Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
title_fullStr Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
title_full_unstemmed Timescales of Growth Response of Microbial Mats to Environmental Change in an Ice-Covered Antarctic Lake
title_sort timescales of growth response of microbial mats to environmental change in an ice-covered antarctic lake
publisher Multidisciplinary Digital Publishing Institute
publishDate 2013
url https://doi.org/10.3390/biology2010151
op_coverage agris
long_lat ENVELOPE(161.917,161.917,-76.150,-76.150)
ENVELOPE(161.600,161.600,-77.517,-77.517)
ENVELOPE(-54.900,-54.900,-61.067,-61.067)
ENVELOPE(161.550,161.550,-77.533,-77.533)
geographic Antarctic
Basin Lake
Lake Vanda
McMurdo Dry Valleys
Pinnacle
Vanda
geographic_facet Antarctic
Basin Lake
Lake Vanda
McMurdo Dry Valleys
Pinnacle
Vanda
genre Antarc*
Antarctic
Antarctica
McMurdo Dry Valleys
genre_facet Antarc*
Antarctic
Antarctica
McMurdo Dry Valleys
op_source Biology; Volume 2; Issue 1; Pages: 151-176
op_relation https://dx.doi.org/10.3390/biology2010151
op_rights https://creativecommons.org/licenses/by/3.0/
op_doi https://doi.org/10.3390/biology2010151
container_title Biology
container_volume 2
container_issue 1
container_start_page 151
op_container_end_page 176
_version_ 1774722174800625664