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1

Distribution of Marenzelleria cf. viridis [Polychaeta: Spionidae] along the Polish coast of the Baltic Sea

100%
Warzocha J., Gromisz S., Wozniczka A., Koper M.
Oceanological and Hydrobiological Studies
|
2005
|
tom 34
|
nr Suppl.1
2

Ultrastructural study and description of Paramyxoides nephtys gen.n., sp.n. a parasite of Nephtys caeca [Fabricius, 1780] [Polychaeta: Nephtyidae]

100%
Larsson J. I. R., Koie M.
Acta Protozoologica
|
2005
|
tom 44
|
nr 2
3
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Biometry and reproductive biology of Pseudonereis anomala Gravier 1901 (Polychaeta: Nereididae) on the Alexandria coast, Egypt

84%
Hamdy R., Dorgham M. M., El-Rashidy H. H., Atta M. M.
Oceanologia
|
2014
|
tom 56
|
nr 1
4

System i filogeneza wieloszczetów (Polychaeta, Annelida) - przegląd koncepcji

84%
Sicinski J.
Przegląd Zoologiczny
|
1991
|
tom 35
|
nr 1-2
5
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Context-dependent consequences of Marenzelleria spp. (Spionidae: Polychaeta) invasion for nutrient cycling in the Northern Baltic Sea

84%
Maximov A., Bonsdorff E., Eremina T., Kauppi L., Norkko A., Norkko J.
Oceanologia
|
2015
|
tom 57
|
nr 4
6

Distribution and abundance of Marenzelleria neglecta [Sikorski and Bick 2004] [Polychaeta, Spionidae] in the Kaliningrad zone of the Baltic Sea in September 2001 and 2002

84%
Gusev A., Starikova I.
Oceanological and Hydrobiological Studies
|
2005
|
tom 34
|
nr Suppl.1
7

The first record of the terrestrial polychaete Hrabeiella periglandulata Pizl et Chalupsky, 1984, in Poland, with a note on anatomy and ecology

84%
Dumnicka E., Rozen A.
Fragmenta Faunistica
|
2002
|
tom 45
|
nr 1
8
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Seasonal changes in the biochemical components of Pseudonereis anomala (Polychaeta, Nereididae) from the Alexandria coast, Egypt

67%
Dorgham M. M., Hamdy R., Al-Rashidy H. H., Atta M. M.
Oceanologia
|
2014
|
tom 56
|
nr 4
9

Malo znani krewniacy dzdzownicy

67%
Jaskula R., Jablonska A.
Wszechświat
|
2005
|
tom 106
|
nr 04-06
132-139
10
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A symbiotic association of a boring polychaete and an echinoid from the Late Cretaceous of Germany

67%
Wisshak M., Neumann C.
Acta Palaeontologica Polonica
|
2006
|
tom 51
|
nr 3
From the Early Maastrichtian white chalk of Rügen Island (N Germany), a specimen of the echinoid Echinocorys ovata featuring 27 boring traces of the ichnogenus Caulostrepsis is described. Individual traces are shallow to moderately deep U−shaped depressions and show distinct regeneration textures evidencing a syn−vivo infestation. All traces are located on the plastron between the peristome and periproct of the host echinoid, indicating an adaptation of the trace maker by choosing the most advantageous position of the specific host. The traces are attributed to the work of boring spionid polychaetes (Polydora complex), grounded on the close morphological resemblance with initial borings of Recent polydorids. This is the first evidence for a possible association of a boring polychaete not only with an echinoid but with an echinoderm in general. The symbiotic relationship was commensalistic in nature with the spionid probably taking advantage of organic matter resuspended by the echinoids locomotion and feeding activity and benefiting from effective shelter. For the host echinoid, the association was moderately harmful. The soft bottom environment of the chalk sea provided very limited hard substrate ecospace for settlers and bioeroders, available only in form of biogenic structures. Echinocorys was a dominant component of this benthic community and can be considered as a suitable host for symbiotic interactions because of its size and assumed longevity.
11

Rurówki - wieloszczety osiadłe

67%
Hapke W.
Nasze Akwarium. Miesięcznik Miłośników i Hodowców Ryb
|
2005
|
nr 04-05[67]
12
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Commensalism in the fossil record: Eunicid polychaete bioerosion on Pliocene solitary corals

67%
Martinell J., Domenech R.
Acta Palaeontologica Polonica
|
2009
|
tom 54
|
nr 1
143-154
Some solitary caryophylliid (Caryophyllia, Trochocyathus, and Ceratotrochus) and flabellid (Flabellum) scleractinian corals from Pliocene of Western Mediterranean exhibit long groove−shaped bioersional structures running along the surface of the thecae. They are epigenic structures produced by an episkeletozoan and therefore, they are described as Fixichnia. Here we propose Sulcichnus as a new ichnogenus, with three new ichnospecies (Sulcichnus maeandriformis, S. helicoidalis, and S. sigillum) to name this traces. Sulcichnus is attributed to the activity of polychaetes. Similar structures are recently produced by Lumbrineris flabellicola, a symbiotic eunicid which maintains a commensalistic relationship with solitary corals. In the fossil record, Sulcichnus occurs associated to shallow marine environments whereas their Recent counterparts are described on deep−marine corals. We interpret this as a consequence of a change in the environmental requirements of the coral/worm pair.
13
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Permian-Triassic scolecodonts and conodonts from the Svalis Dome, Central Barents Sea, Norway

67%
Nakrem H. A., Szaniawski H., Mork A.
Acta Palaeontologica Polonica
|
2001
|
tom 46
|
nr 1
Scolecodonts and conodonts are described from five samples of three cores from the Svalis Dome, central Barents Sea. The conodont species Mesogondolella rosenkrantzi and Neospathodus svalbardensis confirm latest Permian (Dzulfian) and earliest Triassic (Dienerian) ages for the investigated intervals. Correlation with adjacent conodont distribution indicates a shorter depositional gap in the late Permian than is evident on Svalbard. The conodont elements show little thermal alteration with CAI (colour alteration index) values between 1.0 and 1.5 indicating a maximum burial temperature of 50—90°C. The scolecodonts described herein have important evolutionary and distribution implications for polychaetes: the order Eunicida shows a richer diversification in the Permian than previously known; the family Paulinitidae survived at least until the Late Permian; the family Hartmaniellidae diversified already in the late Palaeozoic; some forms are considered as representatives of unknown species and genera; the order Phyllodocida originated already in the latest Palaeozoic.
14

Antarctic neritic zooplankton community [Admiralty Bay, King George Island, South Shetland Islands]

67%
Kittel W., Sicinski J., Zmijewska M. I., Bielecka L., Blachowiak-Samolyk K.
Polish Polar Research
|
2001
|
tom 22
|
nr 1
15

Studies on Oligochaeta taxocens in streams, interstitial and cave waters of Southern Poland with remarks on Aphanoneura and Polychaeta distribution

67%
Dumnicka E.
Acta Zoologica Cracoviensia
|
2000
|
tom 43
|
nr 3-4
16

Small-scale vertical distribution of zoobenthos in the sandy littoral of the Gulf of Gdansk

67%
Haque A. M., Szymelfenig M., Weslawski J. M.
Oceanologia
|
1997
|
tom 39
|
nr 4
17
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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The earliest annelids: Lower Cambrian polychaetes from the Sirius Passet Lagerstatte, Peary Land, North Greenland

67%
Morris S. C., Peel J. S.
Acta Palaeontologica Polonica
|
2008
|
tom 53
|
nr 1
Apart from the Phyllopod Bed of the Burgess Shale (Middle Cambrian) polychaete annelids are practically unknown from any of the Cambrian Lagerstätten. This is surprising both because their diversity in the Burgess Shale is considerable, while to date the Chengjiang Lagerstätte which is equally impressive in terms of faunal diversity has no reliable records of any annelids. Here we describe, on the basis of about 40 specimens, Phragmochaeta canicularis gen. et sp. nov. from the Lower Cambrian Sirius Passet Lagerstätte of Peary Land, North Greenland. This makes it by far the oldest known polychaete, with a likely age of lower to middle Atdabanian, The body consists of approximately 20 segments, each bearing notochaetae and neurochaetae. The former appeared to have formed a felt−like covering on the dorsum, whilst the neurochaetae projected obliquely to the longitudinal axis. Apart from minor differences in chaetal size at either end there is no other tagmosis. Details of the head are obscure, and presence of palps, tentacles and eyes are conjectural. Jaws appear to have been absent. The gut was straight, and flanked by massive longitudinal musculature. P. canicularis was evidently benthic, propelling itself on the neurochaetae, with the dorsal neurochaetae conferring protection. Its stratigraphic position and generalized appearance are consistent with P. canicularis being primitive, but the phylogenetic relationships within the polychaetes remain problematic, principally because of paucity of relevant morphological information.
18

Resources and bottom macrofauna structure in Puck Bay in the 1960 and 1980

59%
Zmudzinski L.
Oceanological Studies
|
1997
|
tom 26
|
nr 1
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