Faunal microfossils: Indicators of Holocene ecological change in a saline Antarctic lake

The sediment record of the fauna of Ace Lake, a saline meromictic lake in the Vestfold Hills, Antarctica, consists of copepod eggs, spermatophores and exoskeletal fragments, rotifer and tintinnid loricae, and foraminiferal and folliculinid tests. The relative abundance of these remains, along with o...

Full description

Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Newman, L, Gibson, JAE, Swadling, KM, Ritz, DA
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science BV 2005
Subjects:
Biological Sciences
Evolutionary Biology
Biogeography and Phylogeography
Ace Lake
Antarctic
Saline Lake
Vestfold
Vestfold Hills
Antarc*
Antarctica
Rotifer
Online Access:https://doi.org/10.1016/j.palaeo.2005.02.005
http://ecite.utas.edu.au/38764
Description
Summary:The sediment record of the fauna of Ace Lake, a saline meromictic lake in the Vestfold Hills, Antarctica, consists of copepod eggs, spermatophores and exoskeletal fragments, rotifer and tintinnid loricae, and foraminiferal and folliculinid tests. The relative abundance of these remains, along with other characteristics of the core, allows the development of a coherent picture of the progress of Ace Lake from a species-poor, freshwater lake early in the Holocene to a biodiverse marine basin following a marine transgression. Subsequent sea level fall reformed Ace Lake as a saline lake and productivity initially increased after isolation. After a major event, possibly associated with overturn of the meromictic lake, biodiversity and productivity decreased, and have continued to do so until the present. 2005 Elsevier B.V. All rights reserved.

Similar Items