Observations on Benthic Larvae of Pareques (Pisces: Sciaenidae) from Florida and Colombia

Copeia ◽  
1978 ◽  
Vol 1978 (1) ◽  
pp. 169 ◽  
Author(s):  
Howard Powles ◽  
Warren E. Burgess
Keyword(s):  
Benthic Larvae

scholarly journals Accumulation and effects of cyanobacterial microcystins and anatoxin-a on benthic larvae of Chironomus spp. (Diptera: Chironomidae)

2014 ◽  
Vol 111 (1) ◽  
pp. 83-90 ◽  
Author(s):  
Magdalena TOPOROWSKA ◽  
Barbara PAWLIK-SKOWRONSKA ◽  
Renata KALINOWSKA
Keyword(s):  
Benthic Larvae

Larval ecology, life history strategies, and patterns of extinction and survivorship among Ordovician trilobites

Paleobiology ◽  
1989 ◽  
Vol 15 (2) ◽  
pp. 118-132 ◽  
Author(s):  
Brian D. E. Chatterton ◽  
Stephen E. Speyer
Keyword(s):  
Life History ◽  
Sea Level ◽  
Significant Loss ◽  
Life History Strategies ◽  
Lower Latitude ◽  
Time Interval ◽  
Larval Ecology ◽  
Planktonic Larvae ◽  
Benthic Larvae ◽  
And Sea Level

Differences in the larval ecology of Ordovician trilobites directly influenced the outcome of the Ashgill extinction (latest Ordovician) and indirectly governed the pattern of evolution in post-Ordovician trilobites. Larval ecology also affected survivorship patterns within the Ordovician, particularly between the Llandeilo and the Caradoc stages. All taxa with pelagic adults became extinct by the end of the Ordovician. Similarly, trilobites with entirely planktonic larvae had all but disappeared by the end of the Ordovician. Although suffering a significant loss in diversity, taxa with benthic larvae provided the ancestral stock for the majority of post-Ordovician lineages. Trilobites with a two-stage protaspid period (single planktonic followed by benthic larvae) suffered least during the Ashgill extinction, giving rise to approximately 23% of the new genera appearing in the early Silurian.Patterns of extinction/survivorship among trilobite taxa with different developmental strategies indicate that the so-called Ashgill extinction was most likely the result of a composite phenomenon, including environmental perturbations, ecosystem breakdown and biogeographic restriction, and was not the consequence of a single catastrophic event (e.g., bolide collision). Indeed, our results are consistent with extinction models which invoke periodic global cooling and sea level regression associated with glaciation. Taxa with planktonic larvae first suffered a marked decline in diversity between the Llandeilo and the Caradoc (end of Middle Ordovician), coincident with the onset of the Ordovician-Silurian glaciation. During this time interval, the paleogeographic ranges of most surviving genera with solely planktonic larvae were severely constricted to lower latitude paleobiogeographic provinces. During the Ashgill (Rawtheyan to Hirnantian), climatic and sea level fluctuations were most extreme because of continued and more extensive glaciation. At this time, when extinctions were particularly severe, there was also a significant effect upon the survivorship of taxa with benthic larvae.Our results indicate that the proportion of the life cycle spent in the water column, dependent upon a planktonic food source, was a critical factor in the survivorship of trilobite taxa during Middle to Late Ordovician time. Consequently, differences in life history patterns predisposed individual taxa to survival or extinction.

scholarly journals A checklist for the zooplankton of the Middle Xingu – an Amazon River system

2015 ◽  
Vol 75 (3 suppl 1) ◽  
pp. 55-64 ◽  
Author(s):  
SAC. Brito ◽  
M. Camargo ◽  
NFAC. Melo ◽  
RA. Estupiñan
Keyword(s):  
Species Richness ◽  
River System ◽  
Main Channel ◽  
Amazon River ◽  
Xingu River ◽  
Benthic Larvae

Abstract A zooplankton checklist is presented for the Middle Xingu River, based on surveys conducted at four sites in the main channel and two fluvial lakes. A total of 175 taxa are listed, including 141 rotifers, 20 cladocerans, and five copepods. Rapids presented the greatest species richness, with up to 124 taxa, while Ilha Grande lake had 70 taxa, the lowest number. Non-planktonic benthic larvae were recorded frequently in the samples.

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