The main source of muddy terrigenous sediment to the central section of the GBR is the Burdekin
|
|
- Pierce Harris
- 5 years ago
- Views:
Transcription
1 Perry 1 Perry et al. Data Repository Items Appendix DR1. Sedimentary Setting The main source of muddy terrigenous sediment to the central section of the GBR is the Burdekin River, located approximately 100 km south of Paluma Shoals. Flows in the Burdekin are highly seasonal (>90% of annual discharge typically occurs between January and April) and variable from year to year, but its mean annual discharge (~ 10 x 10 6 Ml) is the largest entering the Great Barrier Reef (GBR) lagoon. Estimates of mean annual sediment export to the GBR shelf vary from 2.7 Mt (Moss et al. 1983) to 9.0 Mt (Neil and Yu, 1996; Neil et al., 2002). The Ross, Bohle and Black Rivers are important sources of coastal sediment closer to Paluma Shoals, with an average combined annual sediment yield estimated at between Mt (Belperio, 1983). Sediment is transported northwards by longshore wave- and wind-driven currents (Larcombe and Woolfe, 1999), but sediment accumulation rates decrease northwards from the river mouths with long-term accumulation rates of < 0.1 mm yr -1 calculated for Halifax Bay (Woolfe and Larcombe, 1998). The reefs in the vicinity of Paluma Shoals experience prolonged high turbidity events (up to 175 nephelometric turbidity units (NTU) and >40 NTU for more than 40 % of the time) driven by wavedriven resuspension of subtidal terrigenous sediment (Larcombe et al., 2001). This site is appropriate as a location to examine long-term records of coral community response to terrigenoclastic sediment influence and to test the effects of alleged post-european settlement deteriorations in water quality because: (1) The reefs occur within inner-shelf areas that have been a focus for terrigenous sediment accumulation through the mid-late Holocene (Larcombe and Woolfe, 1999), (2) Post-European settlement sediment yields for the proximal Ross and Black Rivers are estimated to be 3 times higher than during pre-european times (Neil et al., 2002),
2 Perry 2 (3) The reefs occur within inner-shelf areas that are episodically influenced by flood plumes (Devlin and Brodie, 2005) and within nearshore zones regarded as at risk from land-derived sediments and nutrients, (4) The site is near other reefs (Havannah and Pandora Reefs, located some 17 km further offshore) where Ba/Ca records in coral skeletons indicate marked increases in sediment influx post-european settlement (McCulloch et al., 2003), and (5) The reefs are located within areas where significant increases in nutrient enrichment in the post- European settlement period have been modelled (Woolridge et al., 2006). References: Belperio, A.P., 1983, Terrigenous sedimentation in the central Great Barrier Reef lagoon: a model from the Burdekin region. BMR Journal of Australian Geolology & Geophysics, v. 8, p Devlin, M. J. and Brodie, J., 2005, Terrestrial discharge into the Great Barrier Reef Lagoon: nutrient behaviour in coastal waters: Marine Pollution Bulletin, v. 51, p Larcombe, P. and Woolfe, K.J., 1999, Terrigenous sediments as influences upon Holocene nearshore coral reefs, central Great Barrier Reef, Australia: Australian Journal of Earth Sciences, v. 46, p Larcombe, P. Ridd, P.V., Prytz, A., and Wilson, B., 1995, Factors controlling suspended sediment on inner-shelf coral reefs, Townsville, Australia: Reefs, v. 14, p McCulloch M., Fallon, S., Wyndham, T., Hendy, E., Lough, J., and Barnes, D., 2003, record of increased sediment flux to the inner Great Barrier Reef since European settlement: Nature, v. 421, p Moss, A., Rayment, G.,Reilly, N., and Best, E., 1983, Sediment and nutrient exports from Queensland coastal catchments: a desk study. Department of Environment and Heritage, Brisbane. Neil, D. and Yu, B., 1996, in H. Hunter, A. Eyles, and G. Rayment, Downstream effects of land use change. Department of Natural Resources, Rockhampton. Neil, D. T., Orpin, A. R., Ridd, P. V., and Yu, B., 2002, Sediment yield and impacts from river catchments to the Great Barrier Reef lagoon: Marine and Freshwater Research, v. 53, p Woolfe, K.J., and Larcombe, P., 1998, Terrigenous sediment accumulation as a regional control on the distribution of reef carbonates, in Camoin, G.F., and Davies, P.J. (Eds.) Reefs and Carbonate Platforms in the Pacific and Indian Oceans. Blackwells, Oxford. pp Wooldridge, S., Brodie, J. and Furnas, M., 2006, Exposure of inner-shelf reefs to nutrient enriched runoff entering the Great Barrier Reef Lagoon: Post-European changes and the design of water quality targets: Marine Pollution Bulletin, v. 52, p
3 Perry 3 Appendix DR2. Materials and Methods 1. Fieldwork and core recovery Core sites were selected to achieve maximum coverage across the reef structure from landward to seaward reef flats. Cores (with the exception of Core PS1/2 recovered using a Jacro 100 system) were recovered using percussion techniques (using aluminium core piping with an internal diameter of 9.5 cm). Cores were up to 2.9 m in length and had 100 % recovery. Rates and depths of core penetration were recorded throughout to ensure a reliable depth chronology and to constrain for sediment compaction (typically ~20%, and which, based on core penetration rates, was uniform down-core). Cores were stored in a cold room after collection. 2. Core logging and sediment facies analysis Recovered cores were split in half using a circular saw to cut through the aluminium pipe, and digital photo composites of each core prepared. Cores were logged to record basic biosedimentary facies information. Data collected included; the ratio of coral clasts to matrix, description of framework fabrics (following Embry and Klovan, 1971), preliminary coral species identification (based on descriptions in Veron and Stafford-Smith, 2002), sediment textural characteristics using the Udden-Wentworth nomenclature, as well as a visual assessment of sediment composition. These criteria were used to delineate basic facies units within the cores (see Fig. 2). Subsequent and more detailed sedimentary analysis included assessments of sediment texture (mean grain size, sorting) and carbonate content based on sub-sampling matrix material at 10 cm downcore intervals. Sediment texture was determined by sieving the 8mm to 63µm size fractions (following the methods in McManus, 1994) and then further analysing the <63µm fraction using a Beckman Coulter Counter. The results of these analyses were combined using the computer programme GRADISTAT (Blott and Pye, 2001), from which values of mean grain size and sorting
4 Perry 4 were taken (descriptive nomenclature of Udden-Wentworth is used throughout). CaCO 3 content was determined from sub-samples of known weight that were treated in a 2M HCl solution until no discernible reaction with the carbonate could be detected. Samples were then filtered through preweighed Whatman 42 filter papers and oven dried. Replicate samples indicated that results were reproducible to within 3%. Carbonate content is reported as % dry weight of the dried original sample. 3. Modern Reef Community Surveys and Taxonomic Analysis of s in Core. Quantitative assessments of contemporary reef community structure were made on an across reef basis based on digital photograph quadrat surveys (10 images per station) undertaken at each of 21 equidistant sampling stations. s were identified to genus level and data grouped into landward, central and seaward zones on the basis of variations in the relative abundance of coral taxa. Data on coral abundance in cores were based on the recovery of all coral material (>1 cm in size) recovered from each 20 cm down-core unit. specimens were examined and grouped based on morphology and skeletal architecture. Each sample group was given a unique identifying code that was used as a basis for recording the composition of all coral material identified in core. samples were subsequently analysed under both binocular and Scanning Electron Microscope (SEM) to examine details of coral microarchitecture and skeletal structure. High-quality coral preservation allowed, in most cases, species-level discrimination (based on reference to taxonomic features in Wallace (1999) and Veron and Stafford-Smith (2002), and reference to the coral collections at the Museum of Tropical Queensland, Townsville). Using this taxonomy, species/genera names were related to material associated with each identifier code and used to examine species abundance down-core. abundance data were analysed in each down-core interval (excluding those that could not be accurately identified either due to size or preservation) and presented as percentage abundance data (see Fig. 2).
5 Perry 5 4. Statistical Treatment of Community Data. One-way Analysis of Similarity (ANOSIM) was used to explore variation in the fossil coral assemblages among depth and time intervals and to compare living communities with fossil assemblages. Because of the difficulty of producing accurate species-level determinations using photo transects, the living coral community data was collected at genus level. Species-level determinations are available for the core record, but except for Acropora (2 species identified), all genera identified were represented by a single species. The first Acropora species (A. muricata) was extremely rare (2 fragments from one sample), and the other species (A. pulchra) was by far the most common taxon in the analysis. Therefore, these two taxa have been merged to enable a genuslevel analysis that is more directly comparable to the composition of living communities. For fossil assemblages, Bray-Curtis dissimilarities were calculated among assemblages recovered from each 20 cm downcore interval using square-root transformed species abundances, rank species abundances, and presence/absence data. Living communities were compared with fossil assemblages calculated from rank abundance and presence/absence data only. All analyses were performed using the R statistical programming language (R_Development_Core_Team, 2006). Four sets of ANOSIM tests were performed. The first set tested the null hypothesis of no significant difference in coral assemblages prior to, and following, changes in land use associated with European settlement. Pre-and post impact cut-offs were placed to bracket a radiocarbon age of cal years BP. This interval occurred at lower levels in landward than seaward cores because of different growth histories across the sampled part of the reef (120 cm in PSS-0 and PSPC1/2, 60 cm in PSS-1, and 40 cm in PSS-2, PS1/2, and PSPC3/4). Using these cut-off values, there was no significant difference among assemblages in the pre-impact and post-impact parts of the cores in analyses of root-transformed absolute abundance (p =0.645), rank abundances (p=0.565) or presence/absence (p=0.415) data. A second set of ANOSIMs were performed to test the null hypothesis of no significant difference of coral assemblages in the top 80 cm of the cores
6 Perry 6 from assemblages in core samples deeper than 80 cm. Tests using log-transformed abundance, rank abundance, or presence/absence data all provided insignificant evidence to reject the null hypothesis suggesting that there was no significant difference in community composition in lower and upper parts of the cores (log abundance p=0.465, rank abundance p=0.255, presence/absence p=0.37). We conclude that no significant change in coral community composition is apparent within the core record since reef initiation. The third and fourth sets of ANOSIMS were designed to compare the composition of the living assemblage with core data from post-impact samples as defined above and samples from the top 80 cm of each core. In each case, analyses performed using both rank abundance and presence/absence provided strong evidence to reject a null hypothesis of no difference between living communities and fossil communities with p-values < Clear differences thus exist between the living reef-flat community and the record of communities preserved in core in both the post-european interval and the shallowest intervals (<80 cm depth) regardless of their age within core. References: Blott, S.J., and Pye, K., 2001, Gradistat: a grain size distribution and statistics package for the analysis of unconsolidated sediments: Earth Surface Processes and Landforms (Technical Communication), v. 26, p Embry, A.F., and Klovan, J.E., A Late Devonian reef tract on northeastern Banks Island, Northwest Territories. Bulletin of Canadian Petrolology and Geology, v. 33, p McManus, J., 1994, Grain size determination, in Tucker, M.E., ed., Techniques in Sedimentology, Blackwells, Oxford, p R_Development_Core_Team., 2006, R: A language and environment for statistical computing, version R Foundation for Statistical Computing, Veron, J. E. N., and Stafford-Smith, M., 2002, ID Key to the zooxanthellate scleractinian corals of the world. CD-Rom, Australian Institute of Marine Sciences, Townsville. Wallace, C., 1999, Staghorn s of the World. CSIRO, Collingwood, Australia, 421 p.
7 Perry 7 Appendix DR3. Radiocarbon Dating of s. Samples selected for radiocarbon dating were sectioned and microsampled to remove surficial calcareous encrustation, washed in distilled water, subjected to ultrasonic agitation in distilled water to remove detrital particles, oven dried (40 o C) and then sealed in plastic bags. Reference is made in the text to a series of radiocarbon-dated cores presented by Smithers and Larcombe (2003), supplemented with a series of additional dates obtained in 2007 (Table 1). Dates were calibrated using Calib and calibration curve Marine04 ( The conventionally employed Marine Reservoir Correction in Australian waters is 450 ± 35 years (Gillespie, 1977). However, various studies have indicated significant deviations in regional marine reservoir signatures. The geographically closest sites to Paluma Shoals are from Port Curtis and Gladstone where marine reservoir ages ranging from 240 ± 61 to 419 ± C y BP are reported (Ulm, 2002). These combined give a weighted mean ΔR value of +10 ± 7, currently the best estimate of variance in the local open water marine reservoir effect for the central Queensland coast (Ulm, 2002). Core number and sample depth. Lab. code Material δ 13 C ratio Conventional 14 C age (years BP) Calibrated (68.2% probability) cal BP PSS1/B1 SUERC ± ± PSS-0-A Wk ± ± PSS-0-B Wk ± ± 54 <60 PSS-0-C Wk ± ± PSS-1-A Wk ± ± PSS-1-B Wk ± ± PSS-1-C Wk ± ± PSS-2-A Wk ± ± PSS-2-B Wk ± ± PSS-2-C Wk ± ±
8 Perry 8 Table DR3. Dates from cores from the South Shoal at Paluma Shoals. Sample SUERC 9967 was dated at the NERC Radiocarbon Dating Laboratory at East Kilbride (UK), the remaining samples at the Waikato Radiocarbon Dating Laboratory in New Zealand. Conventional dates were calibrated using Calib and calibration curve Marine04 ( References: Gillespie, R., 1977, Radiocarbon dating of marine mollusc shells: Australian Quaternary Newsletter v. 9, p Smithers, S. G., and Larcombe, P., 2003, Late Holocene initiation and growth of a nearshore turbidzone coral reef: Paluma Shoals, central Great Barrier Reef, Australia: Reefs, v. 22, p Ulm, S., 2002, Marine and estuarine reservoir effects in Central Queensland, Australia: Determination of the modern marine calibration curve: Geoarchaeology, v. 17, p
9 Perry 9 Appendix DR4 Contemporary Reef Flat Assemblages on the South Shoal at Paluma Shoals. taxa Landward reef flat Central reef flat Seaward reef flat Goniastrea sp Acropora sp Turbinaria sp Galaxea sp Symphyllia sp Lobophyllia sp Favia sp Montipora sp Porites sp Oulophyllia sp Platygyra sp Favites sp Fungia sp Mean live coral cover Table DR4. community data (by coral taxa) and mean live coral cover for each of the distinct zones identified on the reef flat of the South Shoal at Paluma Shoals.
10 Perry 10 Fig. DR4. Contemporary reef flat coral assemblages on the South Shoal at Paluma Shoals. (A) Typical coral communities along the leeward margins of the reef flat that is dominated by extensive low-relief Porites rus pavements and Goniastrea aspera bommies. (B) Detail of leeward reef communities showing colonies of G. aspera, P. rus, Platygyra sp. and Acropora sp. (C) Typical coral communities across the central sections of the reef flat, with abundant G. aspera bommies and extensive carpets of Acropora pulchra. (D) Detail of A. pulchra and a tabular Acropora sp.,
11 Perry 11 both common across the reef flats. (E) Typical coral communities across the central-windward sections of the reef flats, with abundant G. aspera bommies and expansive colonies of Galaxea fascicularis. (F) Details of central-windward reef flat coral communities with colonies of G. fascicularis, Acropora sp., G. aspera and Turbinaria frondens.
Rapid vertical accretion on a 'young' shoredetached turbid zone reef: Offshore Paluma Shoals, central Great Barrier Reef, Australia.
Rapid vertical accretion on a 'young' shoredetached turbid zone reef: Offshore Paluma Shoals, central Great Barrier Reef, Australia. Perry C.T. 1, Smithers S.G. 2 and Gulliver P. 3 1 Geography, College
More informationThis file is part of the following reference: Access to this file is available from:
ResearchOnline@JCU This file is part of the following reference: Costen, Andrew Richard (1996) The sedimentary, hydrodynamic and turbidity regimes at inner shelf coral reefs, Halifax Bay, Central Great
More informationJune 2018 Sediments and Dredging at GBR Ports
June 2018 Sediments and Dredging at GBR Ports Reef 2050 Long Term Sustainability Plan The Great Barrier Reef is over 2000 km long and covers an area of approximately 350,000 square kilometres. It is a
More informationSpatial and temporal patterns of flood plumes in the Great Barrier Reef, Australia
Spatial and temporal patterns of flood plumes in the Great Barrier Reef, Australia Thesis submitted by Michelle Jillian Devlin BSc (Bendigo College of Advanced Education (Latrobe University) Msc (James
More informationPalaeoecological records of coral community development on a turbid, nearshore reef complex: baselines for assessing ecological change
Coral Reefs (217) 36:685 7 DOI 1.17/s338-17-1561-1 REPORT Palaeoecological records of coral community development on a turbid, nearshore reef complex: baselines for assessing ecological change J. A. Johnson
More informationMarine and Tropical Sciences Research Facility Milestone Report, April 2008
Project 3.7.2 Page 1 of 6 Marine and Tropical Sciences Research Facility Milestone Report, April 2008 Program 7: Halting and Reversing the Decline of Water Quality Project 3.7.2: Connectivity and risk:
More informationMarine and Tropical Sciences Research Facility Project Milestone Report
MTSRF Milestone Report Project 3.7.2 Page 1 of 13 Marine and Tropical Sciences Research Facility Project Milestone Report Milestone 3: 8 June 2007 Project 3.7.2: Project Leader: Institution: Connectivity
More informationModelling and monitoring the sediment trapping efficiency and sediment dynamics of the Burdekin Falls Dam, Queensland, Australia
18 th World IMACS / MODSIM Congress, Cairns, Australia 13-17 July 2009 http://mssanz.org.au/modsim09 Modelling and monitoring the sediment trapping efficiency and sediment dynamics of the Burdekin Falls
More informationVariability of nutrient regeneration rates and nutrient concentrations in surface sediments of the northern Great Barrier Reef shelf
Continental Shelf Research 21 (2001) 145 155 Variability of nutrient regeneration rates and nutrient concentrations in surface sediments of the northern Great Barrier Reef shelf M.J. Lourey 1, D.M. Alongi*,
More informationHolocene Carbonate-Siliciclastic Shoreline and Ravinement Stratigraphy of the Belize Lagoon: a Mixed-System Model
Holocene CarbonateSiliciclastic Shoreline and Ravinement Stratigraphy of the Belize Lagoon: a MixedSystem Model DONALD F. MCNEILL AND CLINTON A. COWAN Key findings o Mixedsystem facies heterogeneity during
More informationUsing IKONOS Images to Evaluate Coral Reefs in Low versus High Sedimentation Environments
Using IKONOS Images to Evaluate Coral Reefs in Low versus High Sedimentation Environments David N. Cuevas Miranda Department of Marine Sciences, University of Puerto Rico at Mayagüez P.O. Box 908 Lajas,
More informationModelling and monitoring the sediment trapping efficiency and sediment dynamics of the Burdekin Falls Dam, Queensland, Australia
Lewis, S.E., Sherman, B.S., Bainbridge, Z.T., Brodie, J.E., Cooper, M. (2009). Modelling and monitoring the sediment trapping efficiency and sediment dynamics of the. In Anderssen, R.S., R.D. Braddock
More informationLate Holocene island reef development on the inner zone of the northern Great Barrier Reef: Insights from Low Isles Reef
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in the Earth and Atmospheric Sciences Earth and Atmospheric Sciences, Department of 2008 Late Holocene island reef
More informationSeasonal Changes in the Mekong River Delta's Distributary Channels and Nearshore Sedimentary Environments
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Seasonal Changes in the Mekong River Delta's Distributary Channels and Nearshore Sedimentary Environments Paul Liu & David
More informationTropical river flow and rainfall reconstructions from coral luminescence: Great Barrier Reef, Australia
PALEOCEANOGRAPHY, VOL. 22,, doi:10.1029/2006pa001377, 2007 Tropical river flow and rainfall reconstructions from coral luminescence: Great Barrier Reef, Australia Janice M. Lough 1 Received 11 October
More informationUsing Fossil Coral Reefs from the Seychelles to Understand Past Sea-Level Rise
Using Fossil Coral Reefs from the Seychelles to Understand Past Sea-Level Rise Karen Vyverberg, University of Florida Belinda Dechnik Andrea Dutton Jody Webster Dan Zwartz Future sea-level rise projections
More informationForm 4 of Schedule 5 of the Exclusive Economic Zone and Continental Shelf (Environmental Effects Permitted Activities) Regulations 2013
FORM 4 Permitted activities: Post-activity report Form 4 of Schedule 5 of the Exclusive Economic Zone and Continental Shelf (Environmental Effects Permitted Activities) Regulations 2013 How to use this
More informationContinental shelf records of climate change
Continental shelf records of climate change Wyss W.-S. Yim Guy Carpenter Asia-Pacific Climate Impact Centre, City University of Hong Kong / Department of Earth Sciences, The University of Hong Kong Hong
More informationIII. Acropora coral habitat distribution
2008 Quick Look Report: Miller et al. III. Acropora coral habitat distribution Background The declines in abundance of two of the principal Caribbean reef-building corals, staghorn coral (Acropora cervicornis)
More information(with 3 Text-figures)
18 SUBTIDAL SEDIMENTARY FACIES, SOUTHERN MORETON BAY by M.C. Friederich (with 3 Text-figures) ABSTRACT. On the basis of the mud/sand and carbonate content, sediments are assigned to one of four facies:
More informationThe Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College
The Ocean Floor Chapter 14 Essentials of Geology, 8e Stan Hatfield and Ken Pinzke Southwestern Illinois College The vast world ocean Earth is often referred to as the water planet 71% of Earth s surface
More informationCore Examples from Modern Estuarine Tidal Bars, Tillamook Bay, Oregon
Core Examples from Modern Estuarine Tidal Bars, Tillamook Bay, Oregon Rares Bistran* University of Alberta, Edmonton, Alberta, Canada rares.bistran@ualberta.ca David Herbers, Murray Gingras, John-Paul
More informationMiocene coral reef ecosystems in South East Asia
Miocene coral reef ecosystems in South East Asia Nadia Santodomingo Palaeontology Department Supervisors: Dr. Ken Johnson (NHM) Dr. Lucas J. Lourens (UU) Contents Objectives Fossil Data baseline NTA-2:
More informationSedimentation Dynamics and Stratigraphy of the Middle Breton Sound Estuary, Southeastern Louisiana: Spatiotemporal Evidence for Subdeltaic Evolution
Sedimentation Dynamics and Stratigraphy of the Middle Breton Sound Estuary, Southeastern Louisiana: Spatiotemporal Evidence for Subdeltaic Evolution Edwin J. Bomer IV 1, Samuel J. Bentley 1,2, Kehui Xu
More informationWet season fine sediment dynamics on the inner shelf of the Great Barrier Reef
Wet season fine sediment dynamics on the inner shelf of the Great Barrier Reef Eric Wolanski 1, 2*, Katharina E. Fabricius 1, Timothy F. Cooper 1,2 and Craig Humphrey 1 1 Australian Institute of Marine
More informationSEA BOTTOM MORPHOLOGY AND SEDIMENT DISTRIBUTION OF KUALA BESAR KELANTAN RIVER DELTA AND ITS OFFSHORE AREAS
BORNEO SCIENCE 35: SEPTEMBER 2014 SEA BOTTOM MORPHOLOGY AND SEDIMENT DISTRIBUTION OF KUALA BESAR KELANTAN RIVER DELTA AND ITS OFFSHORE AREAS Nurul Afifah Mohd Radzir* 1, Che Aziz Ali 1, Kamal Roslan Mohamed
More informationRemote Sensing of Episodic Rainfall Events Affecting Coral Reefs in Southwestern Puerto Rico
Remote Sensing of Episodic Rainfall Events Affecting Coral Reefs in Southwestern Puerto Rico Y. Detrés, R. Armstrong, E. Otero and R. García yasmin@cacique.uprm.edu University of Puerto Rico, Mayaguez
More informationThe trapping efficiency of the Burdekin Falls Dam, North Queensland
The trapping efficiency of the Burdekin Falls Dam, North Queensland Estimates from a three-year monitoring program Stephen E. Lewis 1, Zoë T. Bainbridge 1, Bradford S. Sherman 2, Jon E. Brodie 1 and Michelle
More informationLaboratory#6 Sediment Particle Size Distribution and Turbidity Flows
Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows Although this laboratory will pertain to oceanic sediments similar processes can also be observed on land and other aquatic systems
More informationChapter 3 Sedimentation of clay minerals
Chapter 3 Sedimentation of clay minerals 3.1 Clay sedimentation on land 3.2 From land to sea 3.3 Clay sedimentation in the sea 1 3.1 Clay sedimentation on land Deserts Glaciers Rivers Lacustrine 2 University
More informationMicroplastics in the marine environment of coastal British Columbia
Microplastics in the marine environment of coastal British Columbia Jean-Pierre Desforges 1, Moira Galbraith 2, Neil Dangerfield 2, Peter Ross 1 1 School of Earth and Ocean Sciences, University of Victoria,
More informationAltered morphodynamics in tidallyinfluenced rivers: re-thinking catchment management, flood risk & material fluxes
Altered morphodynamics in tidallyinfluenced rivers: re-thinking catchment management, flood risk & material fluxes Paul A. Brewer, Mark G. Macklin, Marc Huband and Sara Rassner Centre for Catchment and
More informationENVIRONMENTAL GEOSCIENCE UNIFORM SYLLABUS
ENVIRONMENTAL GEOSCIENCE UNIFORM SYLLABUS The Association of Professional Engineers and Geoscientists of the Province of British Columbia Note: 1. This Syllabus May Be Subject To Change 2. These Courses
More informationThe Marine Environment
The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write or. 1.
More informationCHAPTER 1 INTRODUCTION
1 CHAPTER 1 INTRODUCTION 1.1 GENERAL Washover sandsheets are often found in low-lying coastal embayment s (Sedgwick and Davis 2003). Washover deposition of marine sand is usually attributed to storm activity
More informationM14/3/GEOGR/SP2/ENG/TZ0/XX/Q GEOGRAPHY STANDARD LEVEL PAPER 2. Monday 19 May 2014 (morning) 1 hour 20 minutes INSTRUCTIONS TO CANDIDATES
M14/3/GEOGR/SP2/ENG/TZ0/XX/Q 22145203 GEOGRAPHY STANDARD LEVEL PAPER 2 Monday 19 May 2014 (morning) 1 hour 20 minutes INSTRUCTIONS TO CANDIDATES Do not open this examination paper until instructed to do
More information3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.
1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments
More information"The Relationship Between Seagrass Cover and Species- richness of Invertebrates"
"The Relationship Between Seagrass Cover and Species- richness of Invertebrates" SCIE 2204: Marine Systems The Cottesloe Marine Ecosystem Research Project 2014 By Baronie Shaw, K., Bortoloso, T., Cargill,
More informationThe Impact of Changing Winds on Estuarine Evolution, Copano Bay, TX
The Impact of Changing Winds on Estuarine Evolution, Copano Bay, TX Purpose: The fulfillment of partial requirements for the Degree of Master of Science in Geology Oklahoma State University, Stillwater
More information(This is a sample cover image for this issue. The actual cover is not yet available at this time.)
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author
More informationSedimentary Environments Chapter 8
Sedimentary Environments Chapter 8 Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. What is a sedimentary rock? Sedimentary rocks are products of
More informationEARTH SURFACE PROCESSES AND SEDIMENTATION!
Sed and Strat EARTH SURFACE PROCESSES AND SEDIMENTATION! 2/27 Lecture 7- Exposure: Weathering and the Sediment Factory 3/04 Lecture 8 - Rivers and Landscapes 3/06 Lecture 9 - Waves (not Tides) 3/11 Lecture
More informationSoil erosion susceptibility and coastal evolution: examples in southern New Caledonia
Pacific Island Countries GIS /RS User Conference Soil erosion susceptibility and coastal evolution: examples in southern New Caledonia Pascal DUMAS et Olivier COHEN University of New-Caledonia (EA 4242/
More informationSmall area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?
The Ocean Basins How Deep is the Ocean? 1 2 Three Major Oceans Three Major Oceans Pacific Atlantic the shallowest ocean (3.3km average depth) Indian second shallowest ocean (3.8km average depth) Pacific
More informationCORAL BIODIVERSITY AND ZONATION ON A PLEISTOCENE REEF, SOUTHEASTERN JAMAICA
CORAL BIODIVERSITY AND ZONATION ON A PLEISTOCENE REEF, SOUTHEASTERN JAMAICA Sherene A. James PhD Student - University of the West Indies, Mona Education Outreach Officer - Natural History Division, Institute
More informationIf it ain t broke, then what? Taphonomic filters of late Pleistocene. Terrestrial Gastropod fossils in the Upper Mississippi Valley
Appendix E 230 If it ain t broke, then what? Taphonomic filters of late Pleistocene Terrestrial Gastropod fossils in the Upper Mississippi Valley Abstract This chapter analyzes terrestrial gastropod shell
More informationThe Coast: Beaches and Shoreline Processes
1 2 3 4 5 6 7 8 9 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions.
More informationLake Levels and Climate Change in Maine and Eastern North America during the last 12,000 years
Maine Geologic Facts and Localities December, 2000 Lake Levels and Climate Change in Maine and Eastern North America during the last 12,000 years Text by Robert A. Johnston, Department of Agriculture,
More informationUnderstanding coastal processes to assist with coastal erosion management in Darwin Harbour, Northern Territory, Australia
IOP Conference Series: Earth and Environmental Science PAPER OPEN ACCESS Understanding coastal processes to assist with coastal erosion management in Darwin Harbour, Northern Territory, Australia To cite
More informationThe Marine Environment
The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write true or
More informationThe Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10
The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions. Identify seasonal
More informationBay of the Living Dead: Preservational Bias and Historical Ecology of Holocene Mollusks in the Chesapeake Bay
Bay of the Living Dead: Preservational Bias and Historical Ecology of Holocene Mollusks in the Chesapeake Bay Rowan Lockwood Department of Geology The College of William & Mary I. Introduction II. III.
More informationChapter 5. The Sedimentary Archives
Chapter 5 The Sedimentary Archives Factors affecting Sedimentary Characteristics 1. Tectonic setting 2. Physical, chemical, and biological processes in the depositional environment 3. Method of sediment
More informationQuaternary corals of Okha- An evidence of Sea level changes and environment of deposition
Indian Journal of Geo-Marine Sciences Vol. 43(7), July 2014, pp. 1260-1265 Quaternary corals of Okha- An evidence of Sea level changes and environment of deposition Pankaj Arpita* & R. L. Jain Geological
More informationProject 1.3.1: Improved knowledge of biota, habitats and risks. Project Leader: Dr Mick Haywood, CSIRO Division of Marine and Atmospheric Research
Marine and Tropical Sciences Research Facility (MTSRF) June 2007 Milestone Report Project 1.3.1: Improved knowledge of biota, habitats and risks Project Leader: Dr Mick Haywood, CSIRO Division of Marine
More informationThe Rare Earth Elements (REEs) from lanthanum to lutetium are members of Group IlIA in the periodic table and all have very similar chemical and
The Rare Earth Elements (REEs) from lanthanum to lutetium are members of Group IlIA in the periodic table and all have very similar chemical and physical properties. REEs along with certain other trace
More informationReefBudget: Introduction and Underpinning Concepts
ReefBudget: Introduction and Underpinning Concepts Funded by: The Leverhulme Trust (International Research Network Programme) Project Contributors: Chris Perry (University of Exeter, UK) Gary Murphy (Manchester
More informationSupplementary Fig. 1. Locations of thinning transects and photos of example samples. Mt Suess/Gondola Ridge transects extended metres above
Supplementary Fig. 1. Locations of thinning transects and photos of example samples. Mt Suess/Gondola Ridge transects extended 260 24 metres above the modern surface of Mackay Glacier, and included 16
More informationEnvironmental Implications A Case Study
Grain Size Variations and Its Environmental Implications A Case Study DR PURANDARA BEKAL SCIENTIST, NATIONAL INSTITUTE OF HYDROLOGY HARD ROCK REGIONAL CENTER HANUMAN NAGAR BELGAUM, KARNATAKA Particle Transport
More informationIII. Distribution and Abundance of Acropora Corals
III. Distribution and Abundance of Acropora Corals Background The declines in abundance of two of the principal Caribbean reef-building corals, staghorn coral (Acropora cervicornis) and elkhorn coral (A.
More informationEcosystem History of Florida Bay and the Southern Estuaries Five Year Update. G. Lynn Wingard (USGS)
Ecosystem History of Florida Bay and the Southern Estuaries Five Year Update G. Lynn Wingard (USGS) Progress since 2003 Florida Bay Science Conference Expansion of Ecosystem History Research into surrounding
More informationRESULTS FROM THE TEXAS COASTAL SEDIMENT SOURCES: A GENERAL EVALUATION STUDY
RESULTS FROM THE TEXAS COASTAL SEDIMENT SOURCES: A GENERAL EVALUATION STUDY JUAN MOYA KELSEY CALVEZ CRIS WEBER ANTHONY RISKO *KEVIN FRENZEL FREESE AND NICHOLS, INC. COASTAL AND WATERWAYS GROUP OBJECTIVES
More informationEarth Science Lesson Plan Quarter 2, Week 10, Day 1
Earth Science Lesson Plan Quarter 2, Week 10, Day 1 Outcomes for Today Standard Focus: PREPARE 1. Background knowledge necessary for today s reading. Beaches are created by the actions of waves, tides,
More informationSediments and Sedimentary Rocks
Sediments and Sedimentary Rocks (Shaping Earth s Surface, Part 2) Science 330 Summer 2005 What is a sedimentary rock? Products of mechanical and chemical weathering Account for about 5 percent of Earth
More informationDiscovery of a large 2.4 Ma Plinian eruption of Basse-Terre, Guadeloupe, from the marine sediment record
GSA Data Repository 2016031 Discovery of a large 2.4 Ma Plinian eruption of Basse-Terre, Guadeloupe, from the marine sediment record Martin R. Palmer et al. Methods Geochemistry 15-25 mg of volcanic grains
More informationHolocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1
Holocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1 Magdy Torab* 2 * Prof. of Geomorphology, Department of Geography, Damanhour University, Egypt 3 E-mail: magdytorab@hotmail.com.
More informationLab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
More informationBrief report on Belize carbonate environments field trip Feb. 2012
Brief report on Belize carbonate environments field trip Feb. 2012 In february 2012 I travelled to San Pedro (Ambergris Caye) Belize (Figure 1) to examine and study depositional environments of carbonate
More informationRecords of climate and vegetation change over time in an area are found from many
Laser Diffraction Particle Size Analysis of Little Lake, Oregon By: Rebecca A Puta, Advisor J Elmo Rawling III Paleolimnology is the study of ancient lake sediments and the significant paleoenvironmental
More informationModelling vulnerability of coastal ecosystems to land-based mining pollution: a case study from Brazil
Modelling vulnerability of coastal ecosystems to land-based mining pollution: a case study from Brazil By Rafael A. Magris, Natalie C. Ban, Jose Monteiro Mining in Brazil is a significant primary industry
More informationWhat creates a coral reef? Why are corals able to form huge reefs?
Marine ecosystems 5: Coral Reefs Unique features The foundation of the ecosystem is produced by living things Reef-building corals Similarities with tropical rain forests Richness and complexity 3-dimensional
More informationAppendix G.19 Hatch Report Pacific NorthWest LNG Lelu Island LNG Maintenance Dredging at the Materials Offloading Facility
Appendix G.19 Hatch Report Pacific NorthWest LNG Lelu Island LNG Maintenance Dredging at the Materials Offloading Facility Project Memo H345670 To: Capt. David Kyle From: O. Sayao/L. Absalonsen December
More informationKamburu Faru Boatu Urunu Faru Velaa Faru Dhakandhoo Mendhoo Funadhoo
IG Working Group REEForm Reef and reef landform responses to environmental and climatic change Report from Research Expedition, Maldives, 29 th June to 13 th July 2011 Participants: hris Perry (Manchester
More informationSupplementary Figure 1. New downcore data from this study. Triangles represent the depth of radiocarbon dates. Error bars represent 2 standard error
Supplementary Figure 1. New downcore data from this study. Triangles represent the depth of radiocarbon dates. Error bars represent 2 standard error of measurement (s.e.m.). 1 Supplementary Figure 2. Particle
More informationFringing and Nearshore Coral Reefs of the Great Barrier Reef: Episodic Holocene Development and Future Prospects
Journal of Coastal Research 22 1 175 187 West Palm Beach, Florida January 2006 Fringing and Nearshore Coral Reefs of the Great Barrier Reef: Episodic Holocene Development and Future Prospects S.G. Smithers,
More informationPaleo Lab #4 - Sedimentary Environments
Paleo Lab #4 - Sedimentary Environments page - 1. CHARACTERISTICS OF SEDIMENT Grain size and grain shape: The sizes and shapes of sedimentary particles (grains) are modified considerably during their transportation
More information2.2.7 Backbarrier flats
FIGURE 24. VERTICAL PHOTOGRAPH SHOWING THE DEVELOPMENT OF SMALL PARABOLIC DUNES FROM BLOWOUTS IN A LARGE RELICT FOREDUNE NORTHWEST OF HUNTER'S CREEK. PHOTOGRAPH COURTESY OF CAR'T'ER HOLT HARVEY FORESTS
More informationControls on fluvial evacuation of sediment from earthquake-triggered landslides
GSA DATA REPOSITORY 2015048 Controls on fluvial evacuation of sediment from earthquake-triggered landslides Jin Wang 1,2,3, Zhangdong Jin 1,4 *, Robert G. Hilton 2, Fei Zhang 1, Alexander L. Densmore 2,5,
More informationCoastal Ocean Circulation Experiment off Senegal (COCES)
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Coastal Ocean Circulation Experiment off Senegal (COCES) Pierre-Marie Poulain Istituto Nazionale di Oceanografia e di Geofisica
More informationIV. Distribution and Abundance of Acropora Corals
IV. Distribution and Abundance of Acropora Corals Background The declines in abundance of two of the principal Caribbean reef-building corals, staghorn coral (Acropora cervicornis) and elkhorn coral (A.
More informationSediment Sources to the Great Barrier Reef what if the coastal zone is a major sediment source rather than a sink?
7 th Australian Stream Management Conference - Full Paper Sediment Sources to the Great Barrier Reef what if the coastal zone is a major sediment source rather than a sink? John Spencer 1, Andrew Brooks
More informationCORAL REEF EVOLUTION AT THE LEEWARD SIDE OF ISHIGAKI ISLAND, SOUTHWEST JAPAN
CORAL REEF EVOLUTION AT THE LEEWARD SIDE OF ISHIGAKI ISLAND, SOUTHWEST JAPAN Hiroya Yamano 1 Osamu Abe 2 Hiroyuki Kitagawa 2 Etsuko Niu 3 Toshio Nakamura 3 ABSTRACT. In comparison with windward coral reefs,
More informationGeology of the Hawaiian Islands
Geology of the Hawaiian Islands Class 12 19 February 2004 A B C D F 97 94 92 91 88 87 86 85 85 84 82 77 73 73 mean 66 64 60 69 60 57 51 29 Exam Scores Mean = 71 Median = 82/77 Any Questions? Sedimentary
More informationJasper Beach, Machiasport, Maine
Maine Geologic Facts and Localities June, 2000 Jasper Beach, Machiasport, Maine 44 o 38 30.28 N, 67 o 22 31.96 W Text by Joesph T. Kelley, Department of Agriculture, Conservation & Forestry 1 Map by USGS
More informationARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!
ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! WHAT PROMINENT FEATURE CAN YOU IDENTIFY IN THIS PICTURE? What do you think the different colors represent? Who might find such a picture
More informationCoral reef degradation is not associated with local human population density
Supplementary Information for: Coral reef degradation is not associated with local human population density John F. Bruno 1 and Abel Valdivia 2 1 Department of Biology, The University of North Carolina
More informationAustralian Mean Sea Level Survey 2009 National Tidal Centre Bureau of Meteorology
Australian Mean Sea Level Survey 2009 National Tidal Centre Bureau of Meteorology Summary There are 39 Australian locations where relative sea levels have been measured for at least 25 years. The average
More informationSetting Priorities for Eelgrass Conservation and Restoration. Robert Buchsbaum Massachusetts Audubon Society
Setting Priorities for Eelgrass Conservation and Restoration Robert Buchsbaum Massachusetts Audubon Society Eelgrass habitat values A rich, productive habitat for many marine organisms Nursery habitat
More informationEarth / Environmental Science. Ch. 14 THE OCEAN FLOOR
Earth / Environmental Science Ch. 14 THE OCEAN FLOOR The Blue Planet Nearly 70% of the Earth s surface is covered by the global ocean It was not until the 1800s that the ocean became an important focus
More informationDepositional Sequences Sequences
Depositional Sequences Transgressive and Regressive packages can be bound by unconformities Because sediment can only be preserved during net aggradation and progradation All other times there is either
More informationOceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface
Oceanography Oceanography is the scientific study of oceans Oceans make up over 70% of the Earth s surface An ocean must be large and have features which set it apart from other oceans (currents, water
More informationLong term in situ observations on typhoon triggered turbidity currents (TC) in the deep sea
Long term in situ observations on typhoon triggered turbidity currents (TC) in the deep sea Article in Geology June 2018 Yanwei Zhang1*, Zhifei Liu1, Yulong Zhao1, Christophe Colin2, Xiaodong Zhang1, Meng
More informationMichael Walsworth, Ryan Sullivan, Simi Odueyungbo, William Budd
Michael Walsworth, Ryan Sullivan, Simi Odueyungbo, William Budd Estuarine Environment At first (Pritchard, 1967), an estuary was defined by the salinity of the water. Then by Clifton (1982) as an inlet
More informationTrace metal contamination of soils and sediments in the Port Kembla area, New South Wales, Australia
University of Wollongong Thesis Collections University of Wollongong Thesis Collection University of Wollongong Year 2009 Trace metal contamination of soils and sediments in the Port Kembla area, New South
More informationCalculating sediment trapping efficiency for Reservoirs in series
22nd International Congress on Modelling and Simulation, Hobart, Tasmania, Australia, 3 to 8 December 2017 mssanz.org.au/modsim2017 Calculating sediment trapping efficiency for Reservoirs in series D.K.
More informationAppendix O. Sediment Transport Modelling Technical Memorandum
Appendix O Sediment Transport Modelling Technical Memorandum w w w. b a i r d. c o m Baird o c e a n s engineering l a k e s design r i v e r s science w a t e r s h e d s construction Final Report Don
More informationESS 312 Geochemistry Lab #6: Biogeochemistry of trace elements and stable isotopes
ESS 312 Geochemistry Lab #6: Biogeochemistry of trace elements and stable isotopes You will have three lab periods to work on this assignment. Late assignments will not be accepted. Read through the lab
More informationMETHODS PAPER: Reservoir Sediment Sampling
Mactaquac Aquatic Ecosystem Study Report Series 2015-003 METHODS PAPER: Reservoir Sediment Sampling A. Chateauvert, B. Wallace, and G. Yamazaki February 10, 2015 Correct citation for this publication:
More informationSediment impacts on coral communities: gametogenesis, spawning, recruitment and early post-recruitment survival Dr Luke Smith
Sediment impacts on coral communities: gametogenesis, spawning, recruitment and early post-recruitment survival Dr Luke Smith AIMS, Fremantle, Western Australia 83 Overview Survival of the different early
More informationModeling the Columbia River Plume on the Oregon Shelf during Summer Upwelling. 2 Model
Modeling the Columbia River Plume on the Oregon Shelf during Summer Upwelling D. P. Fulton August 15, 2007 Abstract The effects of the Columbia River plume on circulation on the Oregon shelf are analyzed
More information