First Mesozoic Scutigeromorph Centipede, from the Lower Cretaceous of Brazil

The first Mesozoic scutigeromorph centipede (Myriapoda: Chilopoda), Fulmenocursor tenax gen. et sp. nov., is described from the Lower Cretaceous (Aptian) Crato Formation of north-east Brazil. Previously described fossil Scutigeromorpha are known from Dominican and Baltic amber, the Carboniferous (Westphalian D) Francis Creek Shale of Mazon Creek, Illinois, the Silurian and Devonian of Britain, and the Devonian of New York State.     

SYSTEMATIC REVISION OF THE SUCKER CREEK AND TROUT CREEK MIOCENE FLORAS OF SOUTHEASTERN OREGON

Graham, Alan. (U. Michigan, Ann Arbor.) Systematic revision of the Sucker Creek and Trout Creek Miocene floras of southeastern Oregon. Amer. Jour. Bot. 50(9): 921–936. Ilus. 1963.—The Sucker Creek flora is preserved in shales of volcanic origin exposed in Malheur County, southeastern Oregon. A study of the flora has been made and the systematic revisions presented. The following new species are described: Osmunda claytonites, Davallia solidités, Shepherdia argen∗∗∗teaites, Magnolia ovulata, Anoda suckerensis, and Platanus youngii. A new combination, Hiraea knowltoni (Berry), is proposed. Additional synonymies, Incertae Sedis, and other taxonomic changes are included. The Trout Creek flora is to the west of Sucker Creek in Harney County, southeastern Oregon. The fossils are preserved in diatomite. Four new species are described: Equisetum miocenicum, Gossypium arnoldii, Urena miocenica, and Spiraea miocenica. New combinations are Pteridium calabazensis (Dorf), and Nymphaea rotunda (Arnold). A revised species list is given for the 2 floras. The Sucker Creek flora contains 47 families, 60 genera, and 69 species, presently identified. The Trout Creek flora contains 29 families, 51 genera, and 75 species. The distributional, ecologic, and geologic interpretations of the 2 floras will be presented in a subsequent publication.     

Salsuginus yutanensis n. sp. (Monogenea: Ancyrocephalidae) from Fundulus sciadicus in Clear Creek of eastern Nebraska

Salsuginus yutanensis n. sp. (Monogenea: Ancyrocephalidae) is described from the gills of the plains topminnow, Fundulus sciadicus Cope, from Clear Creek in eastern Nebraska. Salsuginus yutanensis is distinguished from previously described species by having a shorter accessory piece and different hamulus proportions, especially in the relative lengths of deep and superficial roots. In addition, the angles between deep and superficial roots distinguish S. yutanensis from several congeners.     

Hatching time as an indicator of environmental incompatibility and outbreeding depression in intraspecific salmon hybrids

We analysed hatching times of hybrids between two spatially separated pink salmon Oncorhynchus gorbuscha populations. We repeated the experiment in independent even‐ and odd‐year broodlines. In 1996 and in 1997, we made F1 hybrids from Auke Creek (Juneau, Alaska) females and Pillar Creek (Kodiak, 1000 km away) males and F1 controls from Auke Creek parents. Families were reared and released at Auke Creek. F2 hybrids, controls, and backcrosses were made from F1 returns in 1998 and 1999. In 2001, we made F1 hybrids at Pillar Creek with native females and Auke Creek males. Pillar Creek ancestry prolonged development: At Auke Creek, hybrid families (half Pillar Creek ancestry) developed more slowly (more Accumulated Temperature Units between fertilization and hatch; P  < 0·0001) than did controls (only Auke Creek ancestry). At Pillar Creek, families with only Pillar Creek ancestry developed more slowly than did hybrids with half Auke Creek ancestry. Development times of backcrosses were intermediate between those of hybrids and controls. The variation in development times between Auke Creek and Pillar Creek pink salmon has a genetic component that probably results from local adaptation and illustrates a mechanism that can lead to outbreeding depression in intercrosses between salmon populations ( e.g. , occurring between wild and translocated stocks).     

A synopsis of medullosan pollen organs from the middle Pennsylvanian Mazon creek flora of northeastern Illinois, USA

Six kinds of medullosan pollen organs containing Monoletes-type pollen (prepollen) are described from the middle Pennsylvanian Mazon Creek flora of northeastern Illinois, USA. Codonotheca caduca Sellards and Schopfitheca boulayoides Delevoryas are redescribed and emended diagnoses and new reconstructions are provided. Three forms of Dolerotheca-type pollen organs are described for the first time, along with ultrastructural details of in situ pollen. A sixth kind of pollen organ, tentatively associated with the ovule Stephanospermum konopeonus (Langford) Drinnan, Schramke and Crane, is too poorly preserved for generic assignment but has pollen different from that of other Mazon Creek medullosan pollen organs. This new information on Mazon Creek plants provides important evidence on the diversity of medullosan “pteridosperms” in the flora. Characterization of in situ pollen provides a basis for continuing attempts to associate pollen organs with the variety of co-occuring dispersed ovules.     

ZOSTEROGRAMMIDA, A NEW ORDER OF MILLIPEDES FROM THE MIDDLE SILURIAN OF SCOTLAND AND THE UPPER CARBONIFEROUS OF EURAMERICA

Abstract:  New Palaeozoic millipedes, Zosterogrammus stichostethus gen. et sp. nov. and Casiogrammus ichthyeros gen. and sp. nov., are described from the Francis Creek Shale Member of the Carbondale Formation (Upper Carboniferous: Pennsylvanian), Mazon Creek, Illinois, and the Hagshaw Hills Inlier (Middle Silurian: Wenlock) of the Midland Valley of Scotland, respectively. These millipedes, together with Purkynia lata Fritsch from the Upper Carboniferous (Westphalian D) of Nýřany, Czech Republic, are placed in the new family Zosterogrammidae within the new order Zosterogrammida. All of these millipedes have very broad terga with a microsculpture consisting of fine transverse terrace lines along the anterior of the terga and oblique terrace lines across the remainder. Zosterogrammida have a trunk-ring architecture consisting of an arched diplotergite, a pair of free ventral diplopleurites and a pair of free ventral sternites, indicating a relatively basal phylogenetic position within Chilognatha. Although the exact phylogenetic position is indeterminate, Zosterogrammus stichostethus has divided sternites, indicating a possible affinity with the Pentazonia. The Hagshaw Hills millipede contributes significantly to the high-rank diversity of Middle Silurian millipedes as all previously described taxa of this age belong to the Archipolypoda.     

Upper Ordovician microphytoplankton of the Bill's Creek Shale and Stonington Formation,Upper Peninsula of Michigan,U.S.A.: Biostratigraphy and paleogeographic significance

An abundant, diverse, and well-preserved organic-walled microphytoplankton assemblage is described from the Upper Ordovician Bill's Creek Shale and the lower Stonington Formation (Bay de Noc Member) in the Upper Peninsula of Michigan, U.S.A. Based on graptolite and conodont evidence, the Bill's Creek Shale and Stonington Formation are Richmondian (=Ashgill) in age. The assemblage is dominated by acritarchs, which comprise 29 species (including the enigmatic palynomorph Gloeocapsomorpha prisca) assigned to 20 genera. The prasinophyte phycomata are represented by undifferentiated species of Leiosphaeridia and Tasmanites. In addition, chitinozoans are abundant, and scolecodonts and graptolite fragments are common. Paleontologic-palynologic and sedimentologic evidence indicates that the Bill's Creek Shale was deposited in a low-energy, shallow, nearshore marine environment. The overlying Bay de Noc Member of the Stonington Formation also accumulated in a low-energy, normal marine environment, but in a more offshore, somewhat deeper water setting. Both formations experienced minor transgressive and regressive episodes as indicated by fluctuations in the composition of the palynoflora. The combined Bill's Creek/Stonington acritarch assemblage closely resembles those described from the Richmondian-aged Maquoketa Shale (Missouri and Kansas), Sylvan Shale (Oklahoma), and Vauréal Formation (Anticosti Island, Québec, Canada). The overall composition of the acritarch assemblage from these four formations reflects a distinctive, recognizably Laurentian character. Nonetheless, many of the Bill's Creek/Stonington acritarchs have been reported from Upper Ordovician localities elsewhere, providing additional evidence for Late Ordovician cosmopolitanism of the marine microphytoplankton community. Additionally, the restricted stratigraphic range of many of the taxa further enhances their biostratigraphic application, both regionally and globally, and reaffirms the Richmondian (=Ashgill) age of the Bill's Creek Shale and Stonington Formation.     

A new cephalopod with soft parts from the Upper Carboniferous Francis Creek Shale of Illinois, USA

A ten armed fossil from the Pennsylvanian Francis Creek Shale and belonging to the famous Mazon Creek biota is described as a cephalopod. Apart from a superficial resemblance to the coleoids, there is little basis for an assessment of the animal's affinities. A mineralized Bask shaped structure preserved in calcite and seen in both part and counterpart in fragmentary form may represent the fossilized remains of an internal organ such as the stomach or ink sac A small, dark circular spot positioned anterior to the appendages could be the animal's eye although mere is no internal structure visible. The extremely rare occurrence of Palaeozoic cephalopods with soft parts has so far been Ended to the Francis Creek Shale and the Devonian Hunsrückschiefer of Germany. The Mazon Creek biota includes many fossils which show a remarkable standard of soft part preservation which in some cases includes the fossilization of eye spots and stomach traces. Previously deserted Mazon Creek cephalopods have included the tentacular impression of a squid complete with arm hooks, and the radulae and shells of both coleoids and nautiloids. The specimen described here is the first from the Palaeozoic to show any hint of organ preservation.     

Lignite mining and stream channelization influences on aquatic macroinvertebrate assemblages along the Natchez Trace Parkway,Mississippi, USA

The article describes the effects of channelization on selected water quality parameters and benthic macroinvertebrate assemblages in four Big Black River (Mississippi, USA) tributaries crossing the Natchez Trace Parkway [U.S. National Park Service (NPS)]. Two of the streams were unchannelized (Little Bywy Creek and McCurtain Creek), and two were channelized (Big Bywy Creek and Middle Bywy Creek). Lignite mining occurs in the headwaters of Little Bywy Creek and Middle Bywy Creek. During this 3-year study, benthic macroinvertebrates were collected monthly from all four streams using Hester-Dendy Multiple plate samplers, and enumerated taxonomically and functionally. Hypotheses were tested using analyses of variance. Relationships were determined using multivariate analyses. Relative abundances of mayflies (Ephemeroptera), stoneflies (Plecoptera), caddisflies (Trichoptera) and aquatic beetles (Coleoptera) were associated with moderate to high conductivity, alkalinity, pH, and dissolved oxygen. Hellgrammites (Megaloptera), midges, blackflies, and mosquitoes (Diptera), crayfish (Crustacea: Decapoda) and leeches (Annelida: Hirudinea) were associated with lower values for these parameters. These patterns reflected seasonal rather than spatial variation (i.e., among the streams). Invertebrate assemblage composition was similar among the four streams with respect to functional groups. Invertebrate relative abundances in the two channelized streams were approximately half those of the unchannelized streams. Macroinvertebrate species richness was greater in unchannelized streams. Environmental indices categorized all four streams as having fair to good condition. Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

A new species of Hackelia (Boraginaceae) from Utah

Hackelia ibapensis, a new species of Boraginaceae (Subfamily Boraginoideae, Tribe Eritrichieae) from the Deep Creek Range of Utah is described and illustrated.     

The Response of Three Bacterial Populations to Pollution in a Stream

Abstract Practical methods for biomonitoring of natural systems are still under development. Bacteria are potentially useful indicators of water quality because of their species diversity and ability to rapidly respond to changing environmental conditions. In this study, bacterial populations from unpolluted and polluted stream sites in two watersheds were compared to determine their suitability for use as environmental indicators. Upper Three Runs Creek and Four Mile Creek headwaters have had little anthropogenic disturbance, as opposed to lower Four Mile Creek which received thermal, radioactive, and chemical perturbations. Chemical and physical measurements provided evidence that seepage from holding ponds polluted Four Mile Creek. Polluted sites did not have altered total bacterial numbers but had decreased numbers of colony-forming units. Abundances of three bacterial species, Acinetobacter calcoaceticus, Burkholderia cepacia, and Pseudomonas putida, were determined by colony hybridization with species-specific rDNA probes. Contribution of A. calcoaceticus to the assemblage was higher at polluted sites, which indicated either tolerance of polluted conditions or the ability to utilize compounds existing at these sites to reach larger populations. No differences in B. cepacia populations were detected, and differences in P. putida populations could not be attributed solely to disturbance. The pollution of Four Mile Creek induced differences in bacterial populations that could be monitored using the described approach. Received: 24 September 1996; Accepted: 20 December 1996     

Burbot (Lota lota) exhibit plasticity in life-history traits in a small drainage at the southwestern-most extent of the species' native range

Little is known about the life-history traits exhibited by burbot (Lota lota) throughout their circumpolar range. Monitoring burbot movements between lentic and lotic habits and collection of demographic data (length, age, sex, and maturity) were used to answer the following questions in the Torrey Creek drainage of west-central Wyoming, USA: (a) is there plasticity in the life-history traits of the burbot population, (b) do Trail Lake origin and Torrey Creek origin burbot interchange during the spawning period, and (c) is there a difference in growth and age at sexual maturity between burbot captured in Trail Lake and Torrey Creek? Results indicated that burbot in Trail Lake and Torrey Creek exhibit plasticity in their life history traits. Directional movement of PIT-tagged burbot in Trail Lake and Torrey Creek was monitored nearly continuously by tandem stream-width antennas. Thirty-five percent of lentic-origin burbot migrated upstream into Torrey Creek, and 11% of lotic-origin burbot migrated downstream of the antennas near the Torrey Creek inlet to Trail Lake. Migratory activity of burbot was highest during the late winter and early spring at a time that coincided with spawning. Additionally, Torrey Creek-origin burbot were smaller and younger than Trail Lake-origin burbot. In addition to documenting migration, the sampling of small, sexually mature burbot in Torrey Creek suggests that stream-resident burbot reach maturity earlier than adfluvial and lacustrine burbot in Trail Lake. Furthermore, high catch rates of age-0 burbot indicate that Torrey Creek upstream from Trail Lake provides nursery habitat to the burbot population. Life history trait plasticity and spawning and nursery habitats documented in this study should be considered when selecting conservation actions for this unique burbot population.     

A new species of Late Cretaceous crab (Brachyura: Carcineretidae) from Albion Island, Belize)

A new species of carcineretid crab, Carcineretes planetarius, is described from the Upper Cretaceous (lower Maastrichtian) Barton Creek Dolomite at Albion Island, Belize. The age is based on the stratigraphic range of associated nerineid gastropods and correlation with nannoplankton, benthic foraminifera, and the other known congeneric species of crab found in Jamaica. Confirmation of this age aids in constraining the timing of ejecta deposits of the Chicxulub impact found at the top of Barton Creek Dolomite exposed on Albion Island. Paleoenvironmental and paleoecological analyses suggest that these crabs were swimmers in lagoonal settings, capable of burrowing a few centimeters into the mud for protection.     

<Emphasis Type="Italic">Milax vitukhini</Emphasis>, a new radiolarian species from the Upper Jurassic of the Ust’-Belaya Mountains of the Koryak Upland

A new species, Milax vitukhini sp. nov., from the newly recognized Kimmeridgian–Tithonian radiolarian association from volcanogenic–siliceous–terrigenous rocks of the Borozda Creek Basin (Ust’-Belsky Mountains, Koryak Upland) is described.     

Mapping the Spatial Extent of Depositional Areas in Agricultural,Urban, and Residential California Streams: Implications for Pyrethroid Toxicity

Wetted stream-bed mapping at randomly selected sites in an agricultural stream (Del Puerto Creek), urban stream (Arcade Creek), and residential stream (Pleasant Grove Creek) in California was conducted to determine the spatial extent of depositional and non-depositional areas. This study evaluated the “representativeness” of standard sediment sampling approaches used in California by using hydrophobic pyrethroids as an example. Measured background concentrations of eight pyrethroids in sediment and potential sediment toxicity for each stream were discussed within the context of depositional areas. Four percent, 15%, and 12% of the randomly selected transects in Del Puerto Creek, Arcade Creek, and Pleasant Grove Creek, respectively, were depositional areas. For all three streams, depositional areas were more dominant in downstream segments. Pyrethroid concentrations in sediment were higher in depositional areas versus non-depositional areas in Del Puerto Creek and were also higher downstream. Pyrethroid concentrations in sediment were also higher in downstream areas of Arcade Creek but generally higher in upstream areas of Pleasant Grove Creek. The results from this study demonstrate the importance of determining “representativeness” of depositional areas for an entire stream if hydrophobic chemicals (pyrethroids) measured in sediment from depositional areas are suspected to be toxic.     

A new species of watering pot shell (Bivalvia: Anomalodesmata: Clavagelloidea) from the Miocene of the Murray Basin,South Australia

Abstract: A new species of penicillid watering pot shell, Kendrickiana coquinacola sp. nov., is described from the middle Miocene (Balcombian) Bryant Creek Formation of the Murray Basin, South Australia. The new species differs from the extant K. veitchi in its smaller size, much shorter posterior tube, fewer tubules in the anterior watering pot structure, absence of the pedal slit, discontinuous dorsolateral bands of pitted muscle scars on the internal surface of the anterior bulb and habit of cementing itself to the shells in its surrounding environment. The fossil record of Kendrickiana is reviewed. The record from the Dry Creek Sands is discounted, while a record for the extant K. veitchi from the earliest Pleistocene of York Peninsula is added. K. coquinacola indicates the highly derived anatomy of the genus evolved over a 10‐Ma period from the late Oligocene through the early Miocene.     

Two new brachiopod genera from the Lower Pragian (Lower Devonian,Soda Creek Limestone) of west-central Alaska

New strophomenid and rhynchonellid (Brachiopoda) taxa are described from the Lower Pragian (Soda Creek Limestone) of west-central Alaska: Harperoides gen. nov. with type species H. alaskensis sp. nov. (subfamily Mesodouvillinae Harper et Boucot) and Pedderia gen. nov. with type species P. fragosa sp. nov. (family Pygmaellidae Baranov).     

Thermal regime,predation danger and the early marine exit of sockeye salmon Oncorhynchus nerka

Marine exit timing of sockeye salmon Oncorhynchus nerka populations on the Haida Gwaii Archipelago, British Columbia, Canada, is described, with specific focus on Copper Creek. Marine exit in Copper Creek occurs > 130 days prior to spawning, one of the longest adult freshwater residence periods recorded for any O. nerka population. Copper Creek presents an easy upstream migration, with mild water temperatures (7 to 14° C), short distance (13·1 km) and low elevation gain (41 m) to the lake where fish hold prior to spawning. An energetic model estimates that <1% of the initial energy reserve is required for upstream migration, compared with 62% for lake holding and 38% for reproductive development. Historical records suggest that it is unlikely that water temperature in any of the O.nerka streams in Haida Gwaii has ever exceeded the presumed temperature threshold (19° C) for early marine exit. Although it is not impossible that the thermal tolerance of Copper Creek O.nerka is very low, the data presented here appear inconsistent with thermal avoidance as an explanation for the early marine exit timing in Copper Creek and in three other populations on the archipelago with early marine exit.     

Retention of suspended sediment and phosphorus on a freshwater delta, South Lake Tahoe, California

The Upper Truckee River and Trout Creek, two major tributaries inflowing to Lake Tahoe, join to form what was historically the largest wetland in the Sierra Nevada mountain range that separates California and Nevada (USA). In the 1950s the delta floodplain of the Upper Truckee River was greatly reduced in area (38%) by urban development and the diversion of the river into a single excavated channel. Conversely, Trout Creek still flows through a wide marsh system with significant overbank flooding before entering Lake Tahoe. This study hypothesized that river channel reaches that are not incised within the delta floodplain retain more sediment and nutrients as a result of greater floodplain connectivity, compared to more incised and excavated reaches. Suspended sediment (SS) and total phosphorus (TP) load data from the delta formed by the Upper Truckee River and Trout Creek were collected using flow stage sensors, turbidometers and depth-integrated samples. During the spring snowmelt flow events monitored in 2003, SS load was reduced by 13–41% for the Upper Truckee River and by 68–90% for Trout Creek. Similar reductions in TP load were observed: 13–32% for the Upper Truckee River and 61–84% for Trout Creek. Monitoring of Trout Creek indicated a reduction in load per unit volume of 20–34% in a moderately incised reach versus a reduction of 51–77% in a non-incised marsh reach containing lagoons, braided channels and backwater areas created by a beaver dam. Smaller particle sizes, <10 μm, were retained in the lower marsh reach with similar efficiencies as larger particle sizes. If retention rates from the Trout Creek portion of the marsh are applied to the Upper Truckee River, sediment loading to Lake Tahoe for 2003 would have been reduced by 917 tons of SS.     

Use of NDVI dataset for a GIS based analysis: A sample study of TAR Creek superfund site

Tar Creek is an Environmental Protection Agency (EPA) designated superfund site in Ottawa County, Oklahoma that is heavily polluted with acid mine drainage (AMD) and pollutant deposits in the form of mine tailings (chat piles). Among several residual heavy metal contaminants, zinc and lead are most prevalent in these chat piles. Approximately 50 million cubic yards or 75 million tons of chat remained in Ottawa County as a result of excessive mining in early 1900's to 1960's. This chat is in addition to the pollution that is leached from open mine shafts that drain contaminants into the groundwater, some of which flows directly into streams and creeks. This paper discusses a methodology for incorporating satellite data (MODIS NDVI) within a GIS framework to perform time series analysis in areas near Tar Creek. GIS functions in Map Algebra and Zonal Statistics were implemented to study changes in spectral reflectance due to vegetation at two locations. One of the locations is a sample plot where remedial action consisted of cleaning up of the chat pile and growing native grass. The second location is along Tar Creek and Elm Creek. The paper describes one of the methods that can be used to combine remotely sensed imagery data and spatial feature data within the GIS framework. The main advantages of combining the two datasets using the described process is that, powerful geoprocessing functions within GIS can be easily applied to remote sensing data and the analysis of vector and raster data can be performed in unison.