Exceptional longevity in a lightly exploited, semi‐anadromous clupeid (Perth herring Nematalosa vlaminghi ), within a degraded estuarine environment

2021 ◽  
Author(s):  
Kimberley A. Smith ◽  
Peter G. Coulson ◽  
S. Alex Hesp
Keyword(s):  
Estuarine Environment ◽  
Exceptional Longevity

An adaptive bottlenose dolphin foraging tactic, “shipside feeding,” using container ships in an urban estuarine environment

2021 ◽  
Author(s):  
Meghan Weinpress‐Galipeau ◽  
Hannah Baker ◽  
Bethany Wolf ◽  
Bill Roumillat ◽  
Patricia A. Fair
Keyword(s):  
Bottlenose Dolphin ◽  
Estuarine Environment ◽  
Foraging Tactic

First evidence of an intensive bloom of the coccolithophore Syracosphaera halldalii in a highly variable estuarine environment (Krka River, Adriatic sea)

2021 ◽  
Author(s):  
Sanda Skejić ◽  
Jasna Arapov ◽  
Mia Bužančić ◽  
Živana Ninčević Gladan ◽  
Ana Bakrač ◽  
...  
Keyword(s):  
Adriatic Sea ◽  
Estuarine Environment

Signatures of natural catastrophic events and anthropogenic impact in an estuarine environment, New Zealand

2000 ◽  
Vol 167 (3-4) ◽  
pp. 285-301 ◽  
Author(s):  
C Chagué-Goff ◽  
S.L Nichol ◽  
A.V Jenkinson ◽  
H Heijnis
Keyword(s):  
New Zealand ◽  
Anthropogenic Impact ◽  
Estuarine Environment ◽  
Catastrophic Events

New Early Devonian pteraspidids (Agnatha, Heterostraci) from Death Valley National Monument, southeastern California

1996 ◽  
Vol 70 (1) ◽  
pp. 152-161 ◽  
Author(s):  
David K. Elliott ◽  
Robert R. Ilyes
Keyword(s):  
Estuarine Environment ◽  
Death Valley ◽  
Early Devonian ◽  
National Monument ◽  
Bearing Unit ◽  
Late Emsian

Two species and genera of pteraspidids (Agnatha, Heterostraci), Blieckaspis priscillae n. gen., and Panamintaspis snowi n. gen. and n. sp., together with two undetermined species, are described from the lower part of the Lippincott Member of the Lost Burro Formation, southeastern California. The sharing of similar faunal elements with the Early Devonian assemblages of the Sevy Dolomite and Water Canyon Formation of Utah and Nevada, respectively, together with stratigraphic constraints on the age of the Death Valley fauna, suggest that these assemblages are age equivalent and have a late Emsian (inversus–serotinus Zones) age. The vertebrate-bearing unit of the Lippincott Member is interpreted as a channel-fill deposit laid down in an estuarine environment with low or fluctuating salinity.

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