Out of the doldrums: Campylaspis stephenseni Just, 1970 revived (Crustacea, Cumacea, Nannastacidae)

Similar documents
Contumacious Beasts: A Story of Two Diastylidae (Cumacea) from Arctic Waters

The endemic West African GLYCYMERIDIDAE species. summary and presentation of two new species

'!.t. Deep-Sea Newsletter 20, 12-15, 1993 CHONDROCLADIA GIGANTEA (DEMOSPONGIAE) - THE GIANT CLUBSPONGE OF THE NORTHEAST ATLANTIC

REVIEW OF THE DANISH INVESTIGATIONS ON THE QUANTITATIVE COMPOSITION OP THE BOTTOM FAUNA IN ICELAND AND EAST GREENLAND WATERS

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level.

Bulletin Zoölogisch Museum

A new species of Scherocumella (Crustacea, Cumacea) from a coral lagoon of Lifou, New Caledonia

Preliminary mapping of the distribution of corals observed off West Greenland as inferred from bottom trawl surveys

Canadian Ice Service

APPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1

Seas. A sea is a part of an ocean that is nearly surrounded by water. The Mediterranean, Arctic and Black Sea are really part of the Atlantic Ocean.

Cumacea (Crustacea) from shallow waters of Bermuda

Chapter 02 The Sea Floor

Cumacea (Crustacea) from shallow waters of Bermuda

Laivan nimi Kausi Lähtöpäivä Kohde Risteilyn nimi Midnatsol 18/ EUROPE The Treasures of Portugal Midnatsol 18/ EUROPE

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR

On the world-wide circulation of the deep water from the North Atlantic Ocean

24. Ocean Basins p

A Large Velata from the Lower Jurassic of East Greenland

Wednesday, November 15, 2017

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!

Features of dense water cascades off the Arctic shelves

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY. Lecture 2

Directed Reading. Section: The Water Planet. surface is called the a. Earth s ocean. b. Pacific Ocean. c. salt-water ocean. d. global ocean.

The Marine Environment

by the Bartlett Expedition near the Azores at 37 13'18" N 28 lj'j, 30" W, proved that a related form existed during the Pleistocene ice ages.

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?

ICEBERGS IN THE BARENTS SEA

Oceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface

The Marine Environment

On the Validity of the Name teyahalee as Applied to a Member of the Plethodon glutinosus Complex (Caudata: Plethodontidae): A New Name

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are

Plate Tectonics 3. Where Does All the Extra Crust Go?

Essential Question: How are the geological features that exist on land similar to the geological features on the ocean floor?

3.13Glaciers past and present

24. JURASSIC OSTRACODES OF DEEP SEA DRILLING PROJECT LEG 76, HOLE 534A, BLAKE-BAHAMA BASIN 1

NEW SPECIES OF CUMACEA (CRUSTACEA: PERACARIDA: CUMACEA) FROM BAHAMAS

CALLISPHENUS GRACILIS, N. GEN., N. SP. A FOSSIL ALGA FROM THE WENLOCK OF THE OSLO REGION

OCEANOGRAPHY MEASURING THE DEPTHS OF THE OCEANS

Serial No. N4567 NAFO SCR Doc. 01/178. SCIENTIFIC COUNCIL MEETING November 2001

f r o m a H i g h - R e s o l u t i o n I c e - O c e a n M o d e l

PHYSICAL FEATURES OF EUROPE. Europe Unit

A FOSSIL RIVER BED IN EAST-GREENLAND

The GLYCYMERIDIDAE of the NE Atlantic and the Mediterranean Sea

On the systematic of the water mite Piona annulata (Thor, 1900) (Acari, Hydrachnidia: Pionidae)

28. Genus Xoanon Semenov Fig. C28.1 (female dorsal habitus) Fig. C28.2 (female lateral habitus) Fig. C28.3 (male dorsal habitus)

Redwood City Harbor, California, Navigation Improvement Feasibility Study. Appendix D. Geotechnical Engineering. DRAFT April 2015

Arctic oceanography; the path of North Atlantic Deep Water

Validation of sea ice concentration in the myocean Arctic Monitoring and Forecasting Centre 1

Surface Circulation in the North Atlantic & off of Southern California: Two Models

MARINE GEOLOGY & GEOGRAPHY

Proposed draft marine bioregions

The Ocean Floor Earth Science, 13e Chapter 13

A FOSSIL CRAB FROM THE LAKES ENTRANCE OIL SHAFT, GIPPSLAND, VICTORIA

You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science:

Objectives: Describe the structure of the ocean floor. Describe light intensity and temperature characteristics at different ocean depths.

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens

Lab 7: Sedimentary Structures

(Mollusca, Pholadidae, Xylophagainae) largely confined to depths greater than 150 meters. They are not

A new asellote isopod of the genus Microjanira Schiecke & Fresi, 1970 (Crustacea: Isopoda: Asellota: Janiridae) from Japan

The Arctic Cold War The battle to control resources while the future of the earth hangs in the balance.

UNIT 1: WATER SYSTEMS ON EARTH CHAPTER 2: OCEANS CONTROL THE WATER CYCLE

THE GIANT SPECIES OF THE MOLLUSCAN GENUS LIMA

Climatic Conditions Around Greenland 1995

Seasonal vertical strategies in a high-arctic coastal zooplankton community

Form 4 of Schedule 5 of the Exclusive Economic Zone and Continental Shelf (Environmental Effects Permitted Activities) Regulations 2013

Investigation 5: What happens when plates move sideways past each other?

1. In the block diagram shown here, which is the oldest rock unit?

Surface Circulation in the North Atlantic & off of Southern California: Two Models

Ed Ross 1, David Fissel 1, Humfrey Melling 2. ASL Environmental Sciences Inc. Victoria, British Columbia V8M 1Z5

Euscorpius. Occasional Publications in Scorpiology. Buthus awashensis sp. n. from Ethiopia (Scorpiones: Buthidae) September 2011 No.

Gear data report from Atlantic plankton cruises for the R/V Pathfinder, March March 1962

Ocean Basins, Bathymetry and Sea Levels

Iceberg Plough Marks in the Vicinity of the Norwegian Trough

Chapter 20. Plate Tectonics. Scientific Method. This is a repeatable measurement or experiment. One or more possible explanations to link observations

Gulf Research Reports

Title. Author(s)Lewvanich, Angoon. Issue Date Doc URL. Type. File Information SCHOENOBIINAE)

Amphigomphus somnuki n. sp. from North Thailand (Odonata: Gomphidae) MATTI HAMALAINEN

EKSAMEN i GEO-3121, Marin geologi. Du kan bruke linjal, kalkulator og ordbok! You are allowed to use a ruler, a calculator, and a dictionary!

FEATURES OF TERRIGEN1C MATERIAL TRANSPORT BY ICE IN POLAR SEDIMENTATION

Cruise Report R/V Oceania, AREX 2007

1 / Vol. XXXI 1 pp

Skewed Occurrence Frequency of Water Temperature and Salinity in the Subarctic Regions

CHAPTER 28. PHYSIOGRAPHY Cook Inlet Drainages

Polar Lows and other High Latitude Weather Systems. John Turner and Tom Bracegirdle British Antarctic Survey Cambridge, UK

NAME Lab TA. Introduction to Oceanography, EPSS15 Practice Lecture Exam #1, Fall 2017 Exam#

Evaluation/Monitoring Report No. 259

Where do species names come from?

ON TWO SPECIES OF TERRESTRIAL CRABS OF THE GENUS DROMOTHELPHUSA NAIYANETR, 1992 (CRUSTACEA: DECAPODA: BRACHYURA: POTAMIDAE) FROM THAILAND

We greatly appreciate the thoughtful comments from the reviewers. According to the reviewer s comments, we revised the original manuscript.

Распространение плотных придонных

Ocean Scavenger Hunt. Materials: pencil study notes timer. Directions:

Title The Fauna of Akkeshi Bay : XXII. Phoronidea (With 2. Author(s)Uchida, Tohru; Iwata, Fumio

Polar Lows and Other High Latitude Weather Systems

Question: What is the primary reason for the great abundance of fish along the Peruvian coast?

Earth Science 11 Learning Guide Unit Complete the following paragraph about the ocean and ocean water with the following words:

General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On

The Deep Overflow through the Faroe Bank Channel

VAN AMSTERDAM. S. van der Spoel. C. pyramidata forma convexa (figs. 5-6) was originally. described as a variety found in the Indian

Transcription:

campylaspis stephenseni r e v i v e d Out of the doldrums: Campylaspis stephenseni Just, 1970 revived (Crustacea, Cumacea, Nannastacidae) 45 JEAN JUST Steenstrupia Just, J. Out of the doldrums: Campylaspis stephenseni Just, 1970 revived (Crustacea, Cumacea, Nannastacidae). Steenstrupia 32 (1): 45 50. Copenhagen, Denmark. February 2010. ISSN 0375-2909. Based on type and new material, Campylaspis stephenseni Just, 1970 and C. intermedia Hansen, 1920 are illustrated, and a previously proposed synonymy of the former under the latter name is rejected. The distribution of the two species is discussed. Keywords: Campylaspis stephenseni, C. intermedia, identification, distribution Jean Just, Zoological Museum, Natural History Museum of Denmark, University of Copenhagen, Universitetsparken 15, DK-2100 Copenhagen, Denmark. Email: jean-just@mail.dk INTRODUCTION Species of the nannastacid genus Campylaspis G.O. Sars, with approximately 130 species, are found throughout the world from shallow water to abyssal depths (Watling, 2005), but they are scarce in arctic waters. Up until 1970 only four specimens had been reported from East Greenland: Campylaspis intermedia Hansen, 1920 by Zimmer (1934, Dusénfjord, Franz Joseph Fjord area, 75 185 m, -1.2 C, 2 specimens; material not seen by me) and Campylaspis sp., (Stephensen, 1943, Hurry Inlet, Scoresby Sund area, 2 specimens). Just (1970) described a new species, Campylaspis stephenseni, from Jørgen Brønlund Fjord, Northeast Greenland. At the same time Stephensen s specimens were re-examined. One was found to belong to Campylaspis rubicundum G.O. Sars, a species also reported from Jørgen Brønlund Fjord (Just, 1970). The second specimen belonged to Campylaspis stephenseni. Muradian-Ciamician (1980) reported Campylaspis intermedia from off Beaufort, North Carolina, eastern U.S.A at 344 and 692 m depth. In a very brief and ambiguous note Campylaspis stephenseni Just was, without any explanation, placed in synonymy of Campylaspis intermedia Hansen. In several of the proliferating web based regional check lists the names Campylaspis stephenseni and C. intermedia are used indiscriminately, presumably as a result of Muradian-Ciamician s (1980) synonymisation. The purpose of this note, therefore, is to document, in the simplest way, the differences between Campylaspis intermedia and C. stephenseni, and confirm the latter as a distinctive arctic species so far known from around Greenland only. The distribution of the two species is discussed in a separate section. IDENTIFICATION In Fig.1 Campylaspis stephenseni is documented from north eastern, central eastern, southernmost, and north western Greenland. Apart from the paratype female (Fig. 1B) all specimens are previously unreported, (the specimens are kept in the Zoological Museum, Copenhagen). Collecting data are as follows: Fig. 1A, Jørgen Brønlund Fjord, Peary Land, Northeast Greenland, W of Mundingsholm, 52 m, grey-brown clay, detritus-dredge, Just & Steenstrupia 32 (1): 45 50.

46 j. j u s t Fig. 1. Campylaspis stephenseni Just, 1970. A. Subadult male, Jørgen Brønlund Fjord, lateral and dorsal view. B. Female, paratype, Hurry Inlet, East Greenland. C. Subadult male, Kap Seddon, Northwest Greenland. D. Adult male, Kap Farvel, South Greenland, lateral and dorsal views. Scale = 2 mm. Schiøtte, st. PL16, 14 August 1983. Fig. 1B (paratype), Hurry Inlet, East Greenland, the mouth, 57 m, sandy clay, 30 June 1933 Godthaab st. 43. Fig. 1C, Bay at Kap Seddon, Melville Bay, Northwest Greenland, 75º20.8 N 58º38.6 W, 38 25 m, clay, some sand and gravel, detritusdredge, H. & J. Just, RNV Ingolf st. 5, 4 August

campylaspis stephenseni r e v i v e d 47 Fig. 2. Campylaspis intermedia Hansen, 1920. Syntypes. F. Female, lateral and dorsal views. M. Subadult male, lateral view. Scale = 2 mm. 1980. Fig. 1D, Nua, Kap Farvel area, South Greenland, 59º53.5 N 44º22.3 W, 140 m, stones, gravel, polychaete tubes, triangular dredge, J. Just, Kap Farvel Expedition st. 88, 9 August 1970. The illustrations document a consistent pattern of dorsal and lateral carapace sculpture throughout the known distribution of the species. In females and subadult males there are four dorsolateral keels, (including the dorsoposterior ridge which runs onto the carapace laterally), which merge two-and-two laterally to continue as two single, parallel keels to the ventral front margin. The keels are beset with irregularly spaced rounded knobs. Dorsally, in front of the keels, there are two larger lateral knobs and more medially four smaller knobs in a square. Posteriorly on the dorsal side there are another four smaller knobs arranged in a similar square. The pattern is slightly modified in adult and near adult males (Fig. 1D, and Just 1970, fig. 9a of holotype): the entire carapace is moderately elongate and less deep. The upper posterior branch of the upper lateral keel system is more weakly developed than in the other specimens shown and does not quite connect with the main branch. Younger males (see Fig. 1A) are similar to females. Fig.2 shows a female and a subadult male of Hansen s syntypes of Campylaspis intermedia (material in the Zoological Museum, Natural

48 j. j u s t Fig. 3. Records of Campylaspis stephenseni (circles, T = type locality, holotype) and C. intermedia (squares, S = type localities, syntypes). Black: material seen by the author in preparing this study; open: material not seen. 1, Zimmer 1934; 2, Jones 1984; 3, Vassilenko & Brandt 1996; 4, Gerken & Watling 1999;?, Lomakina 1958.

campylaspis stephenseni r e v i v e d 49 History Museum of Denmark, Copenhagen). The lower lateral keel system is similar to C. stephenseni, but the upper keel does not have a two-pronged posterior part. In addition, there is a vertical, broad keel anteriorly between the upper and lower lateral keels, which is not found in C. stephenseni. The carapace space between the upper and lower keels and behind the vertical keel is broader and deeper than in C. stephenseni. Campylaspis intermedia has the same large dorsolateral knobs but lacks the corresponding four smaller anterior knobs in a square. DISTRIBUTION In addition to the records listed in the Introduction and Identification sections above, the two species in question have been reported as follows: Jones (1984; Fig. 3, 2) reported Campylaspis intermedia from the southern Bay of Biscay. Vassilenko and Brandt (1996; Fig. 3, 3) and Brandt (1997; Fig. 3, 3) listed Campylaspis intermedia (310 321 m depth) and C. stephenseni (45 492 m) from several stations along northeast Greenland from 75 N to 81 N. Gerken and Watling (1999; Fig. 3, 4) reported Campylaspis intermedia (= C. stephenseni Just, 1970) from 15 BioFar stations around the Faroe Islands (225 1319 m). Lomakina (1958, Fig. 3;?) quotes Zimmer (1946, Sedov Reports, in Russian) as reporting Campylaspis intermedia? from Franz Joseph Land and Novaja Zemlya. I have not seen Zimmer s report, but have indicated the possible occurrence in Fig. 3 (?). The depth range of Campylaspis stephenseni as presently known appears to be between 25 and 500 meters, with the species occurring in arctic waters of less than about 2 C. Until the various materials of Campylaspis intermedia listed above have been re-assessed it is not possible to ascertain the depth range and true occurrence of that species, but it seems likely to be present further south and reaching greater depths in the North Atlantic than the former species. DISCUSSION Based on the differences in carapace sculpture the two species are easily separated. Consequently Campylaspis stephenseni Just is removed from synonymy with C. intermedia Hansen and re-instated as a valid species. One question remains: what did Muradian- Ciamician (1980) have to hand when reporting Campylaspis intermedia from off Beaufort, eastern U.S.A.? Muradian-Ciamician (1980: 75; no illustrations provided; no indication that the type materials were examined) writes Although mostly preadult, our specimens certainly belong to this species. As to the whole picture, the one drawn by Just (1970) is more consistent with reality: in Hansen s drawing, the tubercles figured in square section lead to errors [my italics]. Comparison of my illustrations of syntypes of Campylaspis intermedia with Hansen s illustrations (1920, plate III, fig.6) shows that Hansen s rather dark figures, are resonably correct and should not easily lead to error in identification. Hence the Beaufort specimens cannot be Campylaspis intermedia. The reference to Hansen s drawing in square section is uninterpretable. Hansen illustrated a subadult female in lateral and dorsal views, as in my Fig.2A. As to the illustration by Just (1970, fig.9 A) being more consistent with reality, this subjective statement appears to convey only that the Beaufort specimens looked more like Campylaspis stephenseni than C. intermedia. Did Muradian-Ciamician have Campylaspis stephenseni before him? The specimens were collected at 344 and 692 meters depth, so it is marginally possible that this high arctic species could be found on the mid-slope of the western Atlantic. With the difficulties in identification encountered by Muradian-Ciamician, leading to an unjustified synonymization, it is more likely, however, that the Beaufort specimens represent an undescribed species. It is hoped that this short note may provide help in resolving the issue through a re-evaluation of Muradian-Ciamician s material.

50 j. j u s t REFERENCES Brandt, A. 1996. The species composition of the peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya (Greenland). Meddelelser om Grønland, Bioscience 44: 1 30. Brandt, A. 1997. Biodiversity of peracarid crustaceans (Malacostraca) from the shelf down to the deep Arctic Ocean. Biodiversity and Conservation 6: 1533 1556. Gerken, S. & L. Watling. 1999. Cumacea (Crustacea) of the Faroe Island Region. Fróðskaparrit 47: 199 227. Hansen, H. J. 1920. Crustacea Malacostraca IV. The order Cumacea. The Danish Ingolf Expedition III (6): 1 86. Jones, N. S. 1984. The family Nannastacidae (Crustacea: Cumacea) from the deep Atlantic. Bulletin of the British Museum (Natural History), Zoology Series, 46: 207 289. Just, J. 1970. Cumacea from Jørgen Brønlund Fjord, North Greenland. Meddelelser om Grønland 184 (8): 1 23. Lomakina, N. B. 1958. Cumacea of the seas of SSSR. Fauna SSSR 66: 1 301. (In Russian) Muradian-Ciamician, Z. 1980. On some species belonging to the genus Campylaspis (Cumacea, Nannastacidae) from the collections of the Natural History Museum Grigore Antipa. Traveaux du Muséum d Histoire naturelle Grigore Antipa 21: 73 88. Stephensen, K. 1943. Leptostraca, Mysidacea, Cumacea, Tanaidacea, Isopoda, and Euphausiacea. Meddelelser om Grønland 121 (10): 1 82. Vassilenko, S. V. and Brandt, A. 1996. Composition and biogeographic structure of the cumacean fauna of the Northeast Water Polynya, Greenland (Crustacea Peracarida Cumacea). Arthropoda Selecta 5 (3/4): 27 38. Watling, L. 2005. Cumacea World Database. http://marinespecies.org/cumacea. Consulted 2008-08-10. Zimmer, C. 1934. Die Cumaceen der norwegischen Expeditionen nach Ost-Grönland 1929, 1930, 1931 und 1932. Zoological Results of the Norwegian Expedition to East Greenland III. Skrifter om Svalbard og Ishavet 61: 34 40.