Sea Floor Sediments Instructor Guide
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Sediment Activity Answer Key
Sediment Activity Answer Key 1. Were your predictions close to where calcareous and siliceous oozes actually occur? Answers vary. 2. How does your map compare with the sediment distribution map? Answers vary. 3. Which type of ooze dominates the ocean sediments, calcareous or siliceous? Why? Calcareous sediments are formed from the remains of organisms like plankton with calcium-based skeletons1, such as foraminifera, while siliceous ooze is formed from the remains of organisms with silica-based skeletons like diatoms or radiolarians. Calcareous ooze dominates ocean sediments. Organisms with calcium-based shells such as foraminifera are abundant and widely distributed throughout the world’s ocean basins –more so than silica-based organisms. Silica-based phytoplankton such as diatoms are more limited in distribution by their (higher) nutrient requirements and temperature ranges. 4. What parts of the ocean do not have calcareous ooze? What might be some reasons for this? Remember that ooze forms when remains of organisms compose more than 30% of the sediment. The edges of ocean basins bordering land tend to have a greater abundance of lithogenous sediment –sediment that is brought into the ocean by water and wind. The proportion of lithogenous sediment decreases however as you move away from the continental shelf. In nutrient rich areas such as upwelling zones in the polar and equatorial regions, silica-based organisms such as diatoms or radiolarians will dominate, making the sediments more likely to be a siliceous-based ooze. Further, factors such as depth, temperature, and pressure can affect the ability of calcium carbonate to dissolve. Areas of the ocean that lie beneath the carbonate compensation depth (CCD), below which calcium carbonate dissolves, typically beneath 4-5 km, will be dominated by siliceous ooze because calcium-carbonate-based material would dissolve in these regions. -
25. PELAGIC Sedimentsi
^ 25. PELAGIC SEDIMENTSi G. Arrhenius 1. Concept of Pelagic Sedimentation The term pelagic sediment is often rather loosely defined. It is generally applied to marine sediments in which the fraction derived from the continents indicates deposition from a dilute mineral suspension distributed throughout deep-ocean water. It appears logical to base a precise definition of pelagic sediments on some limiting property of this suspension, such as concentration or rate of removal. Further, the property chosen should, if possible, be reflected in the ensuing deposit, so that the criterion in question can be applied to ancient sediments. Extensive measurements of the concentration of particulate matter in sea- water have been carried out by Jerlov (1953); however, these measurements reflect the sum of both the terrigenous mineral sol and particles of organic (biotic) origin. Aluminosilicates form a major part of the inorganic mineral suspension; aluminum is useful as an indicator of these, since this element forms 7 to 9% of the total inorganic component, 2 and can be quantitatively determined at concentration levels down to 3 x lO^i^ (Sackett and Arrhenius, 1962). Measurements of the amount of particulate aluminum in North Pacific deep water indicate an average concentration of 23 [xg/1. of mineral suspensoid, or 10 mg in a vertical sea-water column with a 1 cm^ cross-section at oceanic depth. The mass of mineral particles larger than 0.5 [x constitutes 60%, or less, of the total. From the concentration of the suspensoid and the rate of fallout of terrigenous minerals on the ocean floor, an average passage time (Barth, 1952) of less than 100 years is obtained for the fraction of particles larger than 0.5 [i. -
NPP) A) Global Patterns B) Fate of NPP
OCN 401 Biogeochemical Systems (11.1.11) (Schlesinger: Chapter 9) Oceanic Production, Carbon Regeneration, Sediment Carbon Burial Lecture Outline 1. Net Primary Production (NPP) a) Global Patterns b) Fate of NPP 2. Sediment Diagenesis a) Diagenesis of Organic Matter (OM) b) Biogenic Carbonates Net Primary Production: Global Patterns • Oceanic photosynthesis is ≈ 50% of total photosynthesis on Earth - mostly as phytoplankton (microscopic plants) in surface mixed layer - seaweed accounts for only ≈ 0.1%. • NPP ranges from 130 - 420 gC/m2/yr, lowest in open ocean, highest in coastal zones • Terrestrial forests range from 400-800 gC/m2/yr, while deserts average 80 gC/m2/yr. Net Primary Production: Global Patterns (cont’d.) • O2 distribution is an indirect measure of photosynthesis: CO2 + H2O = CH2O + O2 14 • NPP is usually measured using O2-bottle or C-uptake techniques. 14 • O2 bottle measurements tend to exceed C-uptake rates in the same waters. Net Primary Production: Global Patterns (cont’d.) • Controversy over magnitude of global NPP arises from discrepancies in methods for measuring NPP: estimates range from 27 to 51 x 1015 gC/yr. 14 • O2 bottle measurements tend to exceed C-uptake rates because: - large biomass of picoplankton, only recently observed, which pass through the filters used in the 14C technique. - picoplankton may account for up to 50% of oceanic production. - DOC produced by phytoplankton, a component of NPP, passes through filters. - Problems with contamination of 14C-incubated samples with toxic trace elements depress NPP. Net Primary Production: Global Patterns (cont’d.) Despite disagreement on absolute magnitude of global NPP, there is consensus on the global distribution of NPP. -
Dive Into Oceanography with Trusted Content and Innovative Media
Dive into Oceanography with Trusted Content and Innovative Media The best-selling brief book in the oceanography market combines dynamic visuals and a student-friendly narrative to bring oceanography to life and inspire students to engage and learn more about the oceans and environments around them. The 13th edition creates an interactive learning experience, providing tightly integrated text and digital offerings that make oceanography approachable and digestible for students. An emphasis on the process of science throughout the text provides students with an understanding of how scientists think and work. It also helps students develop the scientific skills of devising experiments and interpreting data. A01_TRUJ1521_13_SE_WALK.indd 1 28/11/2018 13:12 Dive into the Process of Science GraphIt! Activities are a great way to help your students develop their understanding of graphs and data. These activities use real data to help students build science literacy skills and their understanding of how to analyze and interpret graphs. 4.5 What Are the Characteristics of Cosmogenous Sediment? 125 PROCESS OF SCIENCE 4.1: extinction, large outpourings of basaltic did not reveal any K–T deposits. Evidently, When The Dinosaurs Died: volcanic rock in India (called the Deccan the impact and resulting huge waves had Traps) and other locations had occurred. stripped the ocean floor of its sediment. The Cretaceous–Tertiary Also, if there was a catastrophic meteor However, at 1600 kilometers (1000 miles) (K–T) Event impact, where was the crater? from the impact site, the telltale sediments In the early 1990s, the 190-kilometer from the catastrophe, such as the iridium- BACKGROUND (120-mile)-wide Chicxulub (pronounced rich clay layer, were preserved in sea floor The extinction of the dinosaurs—and about “SCHICK-sue-lube”) Crater off the Yu- sediments. -
(Rhizaria) to Biogenic Silica Export in the California Current Ecosystem
Global Biogeochemical Cycles RESEARCH ARTICLE The Significance of Giant Phaeodarians (Rhizaria) 10.1029/2018GB005877 to Biogenic Silica Export in the California Key Points: Current Ecosystem • Phaeodarian skeletons contain large amounts of silica (0.37–43.42 μg Si/ Tristan Biard1 , Jeffrey W. Krause2,3 , Michael R. Stukel4 , and Mark D. Ohman1 cell) that can be predicted from cell size and biovolume 1Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA, 2Dauphin Island Sea Lab, • Phaeodarian contribution to bSiO2 3 4 export from the euphotic zone Dauphin Island, AL, USA, Department of Marine Sciences, University of South Alabama, Mobile, AL, USA, Earth, Ocean, and increases substantially toward Atmospheric Science Department, Florida State University, Tallahassee, FL, USA oligotrophic regions with low total bSiO2 export • Worldwide, Aulosphaeridae alone Abstract In marine ecosystems, many planktonic organisms precipitate biogenic silica (bSiO2) to build fi may represent a signi cant proportion silicified skeletons. Among them, giant siliceous rhizarians (>500 μm), including Radiolaria and Phaeodaria, of bSiO2 export to the deep mesopelagic ocean (>500 m) are important contributors to oceanic carbon pools but little is known about their contribution to the marine silica cycle. We report the first analyses of giant phaeodarians to bSiO2 export in the California Current μ Supporting Information: Ecosystem. We measured the silica content of single rhizarian cells ranging in size from 470 to 3,920 m • Supporting Information S1 and developed allometric equations to predict silica content (0.37–43.42 μg Si/cell) from morphometric • Figure S1 measurements. Using sediment traps to measure phaeodarian fluxes from the euphotic zone on four cruises, • Figure S2 • Figure S3 we calculated bSiO2 export produced by two families, the Aulosphaeridae and Castanellidae. -
Sediment and Sedimentary Rocks
Sediment and sedimentary rocks • Sediment • From sediments to sedimentary rocks (transportation, deposition, preservation and lithification) • Types of sedimentary rocks (clastic, chemical and organic) • Sedimentary structures (bedding, cross-bedding, graded bedding, mud cracks, ripple marks) • Interpretation of sedimentary rocks Sediment • Sediment - loose, solid particles originating from: – Weathering and erosion of pre- existing rocks – Chemical precipitation from solution, including secretion by organisms in water Relationship to Earth’s Systems • Atmosphere – Most sediments produced by weathering in air – Sand and dust transported by wind • Hydrosphere – Water is a primary agent in sediment production, transportation, deposition, cementation, and formation of sedimentary rocks • Biosphere – Oil , the product of partial decay of organic materials , is found in sedimentary rocks Sediment • Classified by particle size – Boulder - >256 mm – Cobble - 64 to 256 mm – Pebble - 2 to 64 mm – Sand - 1/16 to 2 mm – Silt - 1/256 to 1/16 mm – Clay - <1/256 mm From Sediment to Sedimentary Rock • Transportation – Movement of sediment away from its source, typically by water, wind, or ice – Rounding of particles occurs due to abrasion during transport – Sorting occurs as sediment is separated according to grain size by transport agents, especially running water – Sediment size decreases with increased transport distance From Sediment to Sedimentary Rock • Deposition – Settling and coming to rest of transported material – Accumulation of chemical -
Coastal and Shelf Sediment Transport: an Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Coastal and shelf sediment transport: an introduction MICHAEL B. COLLINS 1'3 & PETER S. BALSON 2 1School of Ocean & Earth Science, University of Southampton, Southampton Oceanography Centre, European Way, Southampton S014 3ZH, UK (e-mail." mbc@noc, soton, ac. uk) 2Marine Research Division, AZTI Tecnalia, Herrera Kaia, Portu aldea z/g, Pasaia 20110, Gipuzkoa, Spain 3British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK. Interest in sediment dynamics is generated by the (a) no single method for the determination of need to understand and predict: (i) morphody- sediment transport pathways provides the namic and morphological changes, e.g. beach complete picture; erosion, shifts in navigation channels, changes (b) observational evidence needs to be gathered associated with resource development; (ii) the in a particular study area, in which contem- fate of contaminants in estuarine, coastal and porary and historical data, supported by shelf environment (sediments may act as sources broad-based measurements, is interpreted and sinks for toxic contaminants, depending by an experienced practitioner (Soulsby upon the surrounding physico-chemical condi- 1997); tions); (iii) interactions with biota; and (iv) of (c) the form and internal structure of sedimen- particular relevance to the present Volume, inter- tary sinks can reveal long-term trends in pretations of the stratigraphic record. Within this transport directions, rates and magnitude; context of the latter interest, coastal and shelf (d) complementary short-term measurements sediment may be regarded as a non-renewable and modelling are required, to (b) (above) -- resource; as such, their dynamics are of extreme any model of regional sediment transport importance. -
4. a Growth Model for Polymetallic Nodules
A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐CLIPPERTON FRACTURE ZONE ISA TECHNICAL STUDY SERIES Technical Study No. 1 Global Non‐Living Resources on the Extended Continental Shelf: Prospects at the year 2000 Technical Study No. 2 Polymetallic Massive Sulphides and Cobalt‐Rich Ferromanganese Crusts: Status and Prospects Technical Study No. 3 Biodiversity, Species Ranges and Gene Flow in the Abyssal Pacific Nodule Province: Predicting and Managing the Impacts of Deep Seabed Mining Technical Study No. 4 Issues associated with the Implementation of Article 82 of the United Nations Convention on the Law of the Sea Technical Study No. 5 Non‐Living resources of the Continental Shelf beyond 200 nautical miles: Speculations on the Implementation of Article 82 of the United Nations Convention on the Law of the Sea PAGE | II A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐ CLIPPERTON FRACTURE ZONE This report contains a summary of two documents – A Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone and a Prospector’s Guide prepared under the project ‘Development of a Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone, Pacific Ocean’. ISA TECHNICAL STUDY: NO. 6 International Seabed Authority Kingston, Jamaica PAGE | III The designation employed and the presentation of materials in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the International Seabed Authority concerning the legal status of any country or territory or of its authorities, or concerning the delimitation of its frontiers or maritime boundaries. All rights reserved. -
20. Shell Horizons in Cenozoic Upwelling-Facies Sediments Off Peru: Distribution and Mollusk Fauna in Cores from Leg 1121
Suess, E., von Huene, R., et al., 1990 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 112 20. SHELL HORIZONS IN CENOZOIC UPWELLING-FACIES SEDIMENTS OFF PERU: DISTRIBUTION AND MOLLUSK FAUNA IN CORES FROM LEG 1121 Ralph Schneider2 and Gerold Wefer2 ABSTRACT Shell layers in cores extracted from the continental margin off Peru during Leg 112 of the Ocean Drilling Program (ODP) show the spatial and temporal distribution of mollusks. In addition, the faunal composition of the mollusks in these layers was investigated. Individual shell layers have been combined to form shell horizons whose origin has been traced to periods of increased molluscan growth. It seems that the limiting factor for the growth of mollusks in upwelling regions near the coast of Peru is primarily the oxygen content of the bottom water. Optimal living conditions for mollusks are found at the upper boundary of the oxygen-minimum layer (OML). This OML in the modern sea ranges in depths from 100 to 500 m. Fluctuations in the OML boundary control the spatial and temporal distribution of shell horizons on the outer shelf and upper continental slope. The distribution of mollusks depends further on tectonic events and bottom current effects in the study area. In the range of outer shelf and upper slope, these shell horizons were developed during times of lowered sea level, from the late Miocene through the Quaternary, especially during glacial episodes in the late Quaternary. INTRODUCTION comprehensive reviews of the bivalve and gastropod taxon• omy of the equatorial East Pacific faunal province, but con• Ten holes were drilled using the drill ship JOIDES Reso• tained little information about the ecology of the genera lution during Leg 112, in November and December 1986, on described. -
Ocean Deposits Ocean Deposits Are the Unconsolidated Sediments (Inorganic Or Organic ) Derived from Various Sources Deposited on the Oceanic Floor
Ocean Deposits Ocean deposits are the unconsolidated sediments (Inorganic or Organic ) derived from various sources deposited on the oceanic floor. What are the sources of these ocean deposits ? These ocean deposits are derived from three major sources: 1- Terrigenous Sources 2- Volcanic Deposits 3- Pelagic Deposits What are Terrigenous Deposits ? Weathering is an ongoing process being carried upon,on the various continental rocks by numerous mechanical and chemical agents. As a result of which, these rocks get disintegrated and get decomposed to form fine to coarse sediments.These sediments brought by rivers, streams, winds, glaciers, oceanic currents, waves etc get deposited upon the continental margins are thereby known as terrigenous deposits. The shape and size of these materials differ which in turn influence their seaward distribution. Bigger sized sediments get deposited near the coast such as boulders, cobbles and pebbles, while the finer sediments get deposited away from the sea coast. On the basis of size of particles and density, following pattern has been identified. Deposit Size( Diameter) Gravel 2mm- 256mm Sand 1mm – 1/16mm Silt 1/32mm – 1/256mm Clay 1/256mm – 1/8192mm Mud Finer than 1/8192mm Mud has been further classified into following categories: Type of Mud Characteristics Sediments derived from rocks containing Iron Blue Mud Sulphide and decomposed organic content. Sediments derived from rocks containing Iron Red Mud Oxide Color of blue mud changes into green due to reaction with sea water. It Contains silicates of Green Mud potassium and glauconites Derived from coral reefs located on continental Coral Mud shelf What are Volcanic Deposits ? These are the materials which are deposited in marine environment by volcanic eruptions on land which are carried by wind, river, rain wash etc to the oceans and volcanic eruption in the ocean which deposit sediments directly into the ocean. -
An Improved Cleaning Protocol for Foraminiferal Calcite from Unconsolidated Core Sediments: Hypercal—A New Practice for Micropaleontological and Paleoclimatic Proxies
Journal of Marine Science and Engineering Article An Improved Cleaning Protocol for Foraminiferal Calcite from Unconsolidated Core Sediments: HyPerCal—A New Practice for Micropaleontological and Paleoclimatic Proxies Stergios D. Zarkogiannis 1,2,* , George Kontakiotis 2 , Georgia Gkaniatsa 2, Venkata S. C. Kuppili 3,4, Shashidhara Marathe 3, Kazimir Wanelik 3, Vasiliki Lianou 2, Evanggelia Besiou 2, Panayiota Makri 2 and Assimina Antonarakou 2 1 Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, UK 2 Department of Historical Geology-Paleontology, Faculty of Geology & Geoenvironment, School of Earth Sciences, National & Kapodistrian University of Athens, 157 84 Athens, Greece; [email protected] (G.K.); [email protected] (G.G.); [email protected] (V.L.); [email protected] (E.B.); [email protected] (P.M.); [email protected] (A.A.) 3 Diamond Light Source, Harwell Science and Innovation Campus, Oxford OX11 0DE, UK; [email protected] (V.S.C.K.); [email protected] (S.M.); [email protected] (K.W.) 4 Canadian Light Source, Spectromicroscopy (SM) Beamline, Saskatoon, SK S7N 2V3, Canada * Correspondence: [email protected] Received: 11 November 2020; Accepted: 1 December 2020; Published: 7 December 2020 Abstract: Paleoclimatic and paleoceanographic studies routinely rely on the usage of foraminiferal calcite through faunal, morphometric and physico-chemical proxies. The application of such proxies presupposes the extraction and cleaning of these biomineralized components from ocean sediments in the most efficient way, a process which is often labor intensive and time consuming. In this respect, in this study we performed a systematic experiment for planktonic foraminiferal specimen cleaning using different chemical treatments and evaluated the resulting data of a Late Quaternary gravity core sample from the Aegean Sea. -
Combining Marine Macroecology and Palaeoecology in Understanding Biodiversity: Microfossils As a Model
Biol. Rev. (2015), pp. 000–000. 1 doi: 10.1111/brv.12223 Combining marine macroecology and palaeoecology in understanding biodiversity: microfossils as a model Moriaki Yasuhara1,2,3,∗, Derek P. Tittensor4,5, Helmut Hillebrand6 and Boris Worm4 1School of Biological Sciences, The University of Hong Kong, Pok Fu Lam Road, Hong Kong SAR, China 2Swire Institute of Marine Science, The University of Hong Kong, Cape d’Aguilar Road, Shek O, Hong Kong SAR, China 3Department of Earth Sciences, The University of Hong Kong, Pok Fu Lam Road, Hong Kong SAR, China 4Department of Biology, Dalhousie University, 1355 Oxford Street, Halifax, Nova Scotia, B3H 4R2, Canada 5United Nations Environment Programme World Conservation Monitoring Centre, 219 Huntingdon Road, Cambridge, CB3 0DL, UK 6Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl-von-Ossietzky University of Oldenburg, Schleusenstrasse 1, 26382 Wilhelmshaven, Germany ABSTRACT There is growing interest in the integration of macroecology and palaeoecology towards a better understanding of past, present, and anticipated future biodiversity dynamics. However, the empirical basis for this integration has thus far been limited. Here we review prospects for a macroecology–palaeoecology integration in biodiversity analyses with a focus on marine microfossils [i.e. small (or small parts of) organisms with high fossilization potential, such as foraminifera, ostracodes, diatoms, radiolaria, coccolithophores, dinoflagellates, and ichthyoliths]. Marine microfossils represent a useful model