Please use this identifier to cite or link to this item:
Response of Polytrichum strictum Plants to Regional Warming of the Antarctic Peninsula Using Geochemistry of Past and Modern and Fossil Plants
|Title:||Response of Polytrichum strictum Plants to Regional Warming of the Antarctic Peninsula Using Geochemistry of Past and Modern and Fossil Plants|
|Contributors:||Beilman, David (advisor)|
Global Environmental Science (department)
|Publisher:||University of Hawaiʻi at Mānoa|
|Place of Publication:||Honolulu|
|Abstract:||Ecosystems of the western Antarctic Peninsula (AP) are currently experiencing|
one of the fastest rates of regional warming in the world. Aerobic moss-dominated
peatbanks, which have the most flourishing vegetation in this ice-dominated region, were
studied along the wAP to investigate plant growth conditions over space and time. Living
plants of the dominant moss bank species, Polytrichum strictum, were collected from 13
populations along seven sites located between 6409' and 6735'S and a core was raised
from a Polytrichum-dominated moss bank at 6514’S. Stable isotope ratios were
measured in modern and fossil plant tissue. Modern plant δ
13C values varied from
−31.7 to −27.0‰ and were influenced more by tissue type than geographic location.
Modern plant δ
15N values ranged from −1.4 to +14.7‰ showing little tissue effect. In
the core, radiocarbon-dated fossil leaf tissue showed plant growth began 2300 years ago
(one of the oldest plant ages on the wAP), peat accumulation rates varied over time, and
there is evidence for a hiatus between ~1600 and 800 years ago BP. Fossil leaves
deposited during recent decades had δ13C values between −30.3 and −27.2‰ that were
2.0‰ more depleted than any time during the last 2300 years. Enriched δ15N values of
+11.5 to +13.2‰ in fossil leaves deposited between 209 and 700 years before present
(BP) suggest a period of more trophically-enriched animal inputs. Our results suggest P.
strictum plants have experienced unprecedented growth conditions with recent rapid
warming and that moss bank ecosystems may have changed nutrient sources over time.
|Rights:||All UHM dissertations and theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission from the copyright owner.|
|Rights Holder:||Yumol, Lauren|
|Appears in Collections:||
Global Environmental Science (GES)|
Please email firstname.lastname@example.org if you need this content in ADA-compliant format.
Items in ScholarSpace are protected by copyright, with all rights reserved, unless otherwise indicated.