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Journal articles on the topic 'Intertidal mud-flat'

Author: Grafiati

Published: 3 June 2025

Last updated: 19 July 2025

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1

Lee, Byoung Kwan, Seong Geon Jang, Da Hye Hwang, et al. "Geomorphology and sedimentary environment in the Intertidal zone of Dadohaehaesang National Park." Korea National Park Research Institute 13, no. 1 (2022): 39–47. http://dx.doi.org/10.54406/jnpr.2022.13.1.039.

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To study Geomorphology of intertidal flat around southeastern of Jindo was measurement using terrestrial Lidar and drone and sedimentary environment analysed grain size of surface sediment in the Dadohaehaesang National Park. Compared to average height of intertidal flat was decreased more than 0.1m(2cm/yr) after removed Spartina Alterniflora of invasive salt marsh vegetation species. In southeastern site of intertidal flat before invasive salt marsh vegetation removal was lower height and distributed bimodal/ multimodal of finer mud facies. On the other hand, in northwestern site of intertida

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2

Yamada, Fumihiko, Nobuhisa Kobayashi, Yuichiro Shirakawa, and Yoshihiro Sakanishi. "SEDIMENT BUDGETS BASED ON THE MASS OF SILT AND CLAY ON INTERTIDAL FLAT ADJACENT TO RIVER MOUTH." Coastal Engineering Proceedings 1, no. 32 (2011): 82. http://dx.doi.org/10.9753/icce.v32.sediment.82.

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Fine-grained sediment budgets based on the monthly bed level and net sediment flux monitoring during October 2006 to October 2007 are estimated to examine the relative significance of tides and river discharges on mud transport on an intertidal flat adjacent to a river mouth in the semi-closed sound. The intertidal flat accreted during normal discharge conditions mainly due to the alongshore sediment flux toward the river mouth. However, the flat eroded during large discharge conditions at the time of low tides. The offshore sediment transport during the large discharge was four times larger t

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3

Kim, Il-Hoi. "Poecilostomatoid Copepods from an Intertidal Mud Flat in the Yellow Sea." Journal of Natural History 34, no. 3 (2000): 367–432. https://doi.org/10.1080/002229300299543.

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Kim, Il-Hoi (2000): Poecilostomatoid Copepods from an Intertidal Mud Flat in the Yellow Sea. Journal of Natural History 34 (3): 367-432, DOI: 10.1080/002229300299543, URL: http://www.tandfonline.com/doi/abs/10.1080/002229300299543

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4

Riaux-Gobin, Catherine. "The diatom genus Cocconeis from an intertidal mud flat of North Brittany: source and diversity." Canadian Journal of Botany 69, no. 3 (1991): 597–601. http://dx.doi.org/10.1139/b91-081.

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A 1 -year survey of an epipelic diatom assemblage from a North Brittany marine mud flat revealed the presence of 23 species of Cocconeis. About 10 of these species were common, and the remaining ones were rare. These species of Cocconeis for the most part have small dimensions (nannophytobenthos). The species collected from the intertidal sediment, the specific richness, and seasonal occurrences are compared with those of an epiphytic assemblage on Zostera marina L. from the same region. Key words: benthic diatoms, Cocconeis, North Brittany, mud flat.

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5

Lathrop, Richard G., Daniel Merchant, Larry Niles, et al. "Multi-Sensor Remote Sensing of Intertidal Flat Habitats for Migratory Shorebird Conservation." Remote Sensing 14, no. 19 (2022): 5016. http://dx.doi.org/10.3390/rs14195016.

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Many species of shorebirds migrate long distances from their overwintering grounds in the southern hemisphere to breeding grounds in the northern hemisphere. The coastal intertidal zone, consisting of sand and mud flats exposed at low tide and covered at high tide, is heavily used as a migratory stopover or overwintering habitat. Understanding the spatial distribution of sediment types at these stopover sites is a critical step for understanding habitat use by shorebird species. Due to their importance as overwintering and stopover habitat for the imperiled western Atlantic subpopulation of th

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6

Uzaki, Ken-ichi, Yoshiaki Kuriyama, and Hikari Sakamoto. "NUMERICAL STUDY OF THE MORPHODYNAMIC CHANGE OF INTERTIDAL FLATS DUE TO TIDAL AND COASTAL CURRENTS." Coastal Engineering Proceedings 1, no. 32 (2011): 51. http://dx.doi.org/10.9753/icce.v32.sediment.51.

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Numerical model of the morphodynamic change of intertidal flats is very important to maintain intertidal flats and construct artificial flats. In this study, three-dimensional morphodynamic model considering tidal and coastal currents, sand and cohesive sediments was developed and applied to the Shirakawa intertidal flat in the Ariake Sea in Japan. From comparisons between numerical and observation results around the rivermouth of Shirakawa River, we could recognize the qualitative validity of the numerical model. Furthermore, the simultaneous simulation of tidal and coastal currents and the i

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7

Iqbal, Faiza, Kurt Auffenberg, Safia Khanam, and Javed Mustaquim. "Rediscovery and Redescription of Snail Pupoides karachiensis Peile, 1929 (Gastropoda: Pupillidae) with Notes on P. coenopictus (Hutton, 1834) from the Karachi Tidal Marsh." Tropical Natural History 23 (March 28, 2023): 52–55. https://doi.org/10.58837/tnh.23.1.258420.

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Pupoides karachiensis Peile, 1929 was described from beach sand taken from near Karachi (then British India, now Pakistan). To our knowledge this species has not been reported in the scientific literature for 92 years. During an ecological survey of intertidal mud flat of Korangi Creek, Karachi, we found specimens of P. karachiensis associated with P. coenopictus (T. Hutton, 1834). This is the first subsequent record of P. karachiensis since Pilsbry (1931) and we take the opportunity to redescribe the species and include notes on P. coenopictus. Shell measurements and the distributions of shel

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8

Shone, Russell W. "A new ophiuroid from the Sundays River Formation (Lower Cretaceous), South Africa." Journal of Paleontology 60, no. 4 (1986): 904–10. http://dx.doi.org/10.1017/s0022336000043067.

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Ophiolancea swartkopensis n. gen. and sp. is the first ophiuroid to be described from the Lower Cretaceous (Valanginian) Sundays River Formation, South Africa. Ophiolancea is distinguished by lanceolate lateral arm shields which occur on the distal portions of the arms. Associated fauna and stratigraphic evidence suggest that the specimen was buried in an intertidal mud flat.

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9

Kim, Il-Hoi. "Poecilostomatoid Copepods from an Intertidal Mud Flat in the Yellow Sea." Journal of Natural History 34, no. 3 (2000): 367–432. http://dx.doi.org/10.1080/002229300299543.

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10

Mouritsen, Kim N., and Robert Poulin. "The mud flat anemone-cockle association: mutualism in the intertidal zone?" Oecologia 135, no. 1 (2003): 131–37. http://dx.doi.org/10.1007/s00442-003-1183-x.

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11

Liu, Kang Ning, Zai Xing Jiang, Da Kang Zhong, Rong Kang, and Yue Cao. "Study on Sedimentary Facies of Carboniferous Kalashayi Formation in the South of Tahe Oilfield." Advanced Materials Research 433-440 (January 2012): 1745–50. http://dx.doi.org/10.4028/www.scientific.net/amr.433-440.1745.

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Tahe Oilfield is an significant petroleum exploitation and development area in Tarim Basin for SINOPIC. Carboniferous Kalashayi Formation has become an important oil-bearing series for increasing and maintaining production, and for finding backup resource in this Oilfield. Based on the theories and methods of sedimentology, by using the sesmic, log and core data, the sedimentary facies of Carboniferous Kalashayi Formation in the south of Tahe Oilfield are analyzed deeply. Through the study of characteristics of the rock type and texture,sedimentary structure, sedimentary sequence, stratic stru

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12

Chu, Diarmuid. "Sampling in Shenzhen Bay: Biodiversity and environment." Young Scientist 3, no. 1 (2024): 29–32. https://doi.org/10.5281/zenodo.10935362.

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Shenzhen Bay was originally mud flat, but the coastline of nowadays days' Shenzhen Bay was artificial. In this summer, a sampling was done for studying the biodiversity of Shenzhen Bay. The sampling started in Shenzhen Bay at 5 P.M. which was the time that intertidal zone started to exist. The intertidal zone of Shenzhen was mostly composed of mud flats. Only the part beside the beach was filled with rocks. This feature is due to land reclamation, so that the original habitats of marine organisms were destroyed. The components of Shenzhen Bay's bio-community were mostly crabs, mudskipper, sea

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13

Mangano, Gabriela M., Luis A. Buatois, Ronald R. West, and Christopher G. Maples. "Ichnology of a Pennsylvanian Equatorial Tidal Flat -- The Stull Shale Member at Waverly, Eastern Kansas." Bulletin (Kansas Geological Survey), no. 245 (January 1, 2002): 1–139. https://doi.org/10.17161/kgsbulletin.no.i245.22279.

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Integrated stratigraphic, sedimentologic, and ichnologic analyses indicate that the Stull Shale Member (Kanwaka Shale, Shawnee Group) at Waverly (Coffey County, eastern Kansas) was deposited along a microtidal shoreline directly connected with the open sea and outside of a northeast-south west-oriented embayment. Six major subenvironments have been identified in the lower interval of the Waverly section: sand flat, mixed flat, mud flat, supratidal paleosols, intertidal runoff channels, and fluvial channel. Paleogeographic information indicates that the position of the Waverly tidal flat was eq

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14

Peterson, Curt D., and Sandy Vanderburgh. "Tidal Flat Depositional Response to Neotectonic Cyclic Uplift and Subsidence (1–2 m) as Superimposed on Latest-Holocene Net Sea Level Rise (1.0 m/ka) in a Large Shallow Mesotidal Wave-Dominated Estuary, Willapa Bay, Washington, USA." Journal of Geography and Geology 10, no. 1 (2018): 109. http://dx.doi.org/10.5539/jgg.v10n1p109.

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The late-Holocene record of tidal flat deposition in the large shallow Willapa Bay estuary (43 km in length), located in the Columbia River Littoral Cell (CRLC) system (160 km length), was investigated with new vibracores (n=30) and gouge cores (n=8), reaching 2–5 m depth subsurface. Reversing up-core trends of muddy sand to peaty mud deposits in marginal tidal flat settings demonstrate episodic submergence events resulting from cyclic tectonic uplift and subsidence (1–2 m) in the Cascadia subduction zone. These short-term reversals are superimposed on longer-term trends of overall sediment co

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15

Sanders, Christian J., Joseph M. Smoak, A. Sathy Naidu, Luciana M. Sanders, and Sambasiva R. Patchineelam. "Organic carbon burial in a mangrove forest, margin and intertidal mud flat." Estuarine, Coastal and Shelf Science 90, no. 3 (2010): 168–72. http://dx.doi.org/10.1016/j.ecss.2010.08.013.

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16

Yamada, F., N. Kobayashi, Y. Shirakawa, Y. Watabe, S. Sassa, and A. Tamaki. "Effects of Tide and River Discharge on Mud Transport on Intertidal Flat." Journal of Waterway, Port, Coastal, and Ocean Engineering 138, no. 2 (2012): 172–80. http://dx.doi.org/10.1061/(asce)ww.1943-5460.0000108.

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17

Cranford, Peter J. "Behaviour and ecological importance of a mud snail (Ilyanassa obsoleta) population in a temperate macrotidal estuary." Canadian Journal of Zoology 66, no. 2 (1988): 459–66. http://dx.doi.org/10.1139/z88-065.

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A population of Ilyanassa obsoleta was sampled during the 8-month period when they are present in the intertidal zone in the Southern Bight of Minas Basin, Bay of Fundy. Mud snails were first observed in April, and spawning took place in late May and early June. Flesh weight increased between May and November, with the highest growth rates recorded during August and September. During November the population returned to the subtidal zone, where energy reserves are partially utilized during winter. Clustering and differential habitat selection (salt marsh or mud flat) within size classes resulte

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18

Vargas, José A. "A survey of the meiofauna of an Eastern Tropical Pacific intertidal mud flat." Revista de Biología Tropical 36, no. 2B (2016): 541–44. http://dx.doi.org/10.15517/rbt.v36i2b.23894.

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19

Hamilton, Diana J., Myriam A. Barbeau, and Antony W. Diamond. "Shorebirds, mud snails, and Corophium volutator in the upper Bay of Fundy, Canada: predicting bird activity on intertidal mud flats." Canadian Journal of Zoology 81, no. 8 (2003): 1358–66. http://dx.doi.org/10.1139/z03-130.

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The upper Bay of Fundy is a critical staging area for migrating semipalmated sandpipers (Calidris pusilla), which feed extensively on the amphipod Corophium volutator. Recent changes in the distributions of birds around the bay have generated interest in understanding the factors that influence shorebirds' habitat use. To examine some of these factors, we surveyed four mud flats during summer 2000. Abundance of shorebirds and density of C. volutator and mud snails (Ilyanassa obsoleta) were assessed in two focused areas and on two broad-scale transects per mud flat. Shorebird abundance varied w

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20

KOMAI, TOMOYUKI, and YOSHIHISA FUJITA. "A new species of the mud shrimp genus Axianassa Schmitt, 1924 (Decapoda: Gebiidea: Laomediidae) from the Ryukyu Islands, southern Japan." Zootaxa 4658, no. 3 (2019): 452–60. http://dx.doi.org/10.11646/zootaxa.4658.3.2.

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A new species of the laomediid mud shrimp genus Axianassa Schmitt, 1924, A. planioculus, is described and illustrated on the basis of a single male specimen from intertidal muddy sand flat of Kabira Bay, Ishigaki Island, southern Ryukyu Islands, Japan. Axianassa planioculus n. sp. is morphologically closest to A. mineri Boone, 1931, known from Pacific Panama, among the 11 known congeners, but is readily distinguished from the latter by the eyes being dorsally concealed by the rostrum, the subovate telson, the unarmed carpus of the maxilliped 3 and the unarmed uropodal endopod. The discovery of

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21

Sprung, Martin. "Observations on the life cycle of Abra ovata on an intertidal mud flat in portugal." Journal of the Marine Biological Association of the United Kingdom 74, no. 4 (1994): 919–25. http://dx.doi.org/10.1017/s0025315400090147.

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On an intertidal mud flat in the Ria Formosa (southern Portugal) Abra ovata (Mollusca: Bivalvia) showed effective meiobenthic and macrobenthic dispersal (i.e. of individuals smaller and larger than 1 mm). This was important to compensate for mortality caused by shore crabs during summer. It was observed in the laboratory that A. ovata deposited eggs in capsules on the sediment surface; after 11–15 d at 20°C benthic juveniles of 210–220 (im shell length hatched from these capsules. A pelagic larval stage was missing. Large numbers of specimens of about 1 mm shell length colonized protected buck

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22

Sawicka, Joanna E., Alberto Robador, Casey Hubert, Bo Barker Jørgensen, and Volker Brüchert. "Effects of freeze–thaw cycles on anaerobic microbial processes in an Arctic intertidal mud flat." ISME Journal 4, no. 4 (2009): 585–94. http://dx.doi.org/10.1038/ismej.2009.140.

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23

Gibran, Akhmad Khahlil, and Aries Kusworo. "FASIES DAN LINGKUNGAN PENGENDAPAN FORMASI KANIKEH, CEKUNGAN BULA, MALUKU." RISET Geologi dan Pertambangan 30, no. 2 (2020): 171. http://dx.doi.org/10.14203/risetgeotam2020.v30.1108.

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Batuan silisiklastik berumur Trias yaitu Formasi Kanikeh, tersebar di Pulau Seram hingga Pulau Kesui dan Teor dari Maluku hingga Maluku Tenggara. Formasi Kanikeh telah lama dikenal memiliki karakteristik batuan induk yang baik. Pemahaman tentang Formasi Kanikeh masih minim, interpretasi lingkungan pengendapan dan korelasi stratigrafi masih ada perbedaan. Tujuan penelitian ini adalah mendapatkan hasil interpretasi lingkungan pengendapan berdasarkan data terbaru. Metode yang digunakan dalam penelitian ini adalah pengukuran penampang stratigrafi pada empat lintasan pengamatan di daerah Seram Bagi

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24

ZHENG, WENBO, and HONGWEN DENG. "High-resolution sequence stratigraphic division and distribution of tidal deposits in the Zhuhai Formation, Huizhou Sag, Pearl River Mouth Basin, South China Sea." Geological Magazine 149, no. 4 (2011): 722–28. http://dx.doi.org/10.1017/s0016756811000768.

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AbstractThe Zhuhai Formation of the Huizhou Oilfield has been interpreted as being deposited in a tide-dominated estuarine setting. This paper uses stratigraphic principles, cores and logging data to analyse the facies changes of tidal sedimentation in response to the base level cycle. We conclude that the mud flat progradational allocycle is the result of a long-term base level fall, while the fining-upwards autocycle is in response to a short-term base level fall. Region-wide mud layers of supratidal zones and scour surfaces of subtidal zones are stratigraphic surfaces of tidal sedimentation

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25

Peterson, Curt D., and Sandy Vanderburgh. "Interconnected Accommodation Space Controls Between Sand-Charged Shallow Tidal Channels and Wind-Wave Truncated Tidal Flats During Latest-Holocene Sea Level Rise (~3.0 m) in a Large Mesotidal Wave-Dominated Estuary, Grays Harbor, Washington, USA." Journal of Geography and Geology 10, no. 3 (2018): 26. http://dx.doi.org/10.5539/jgg.v10n3p26.

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The late-Holocene (5–0 ka) record of accommodation space controls of tidal channel and tidal flat deposition in the shallow mesotidal wave-dominated Grays Harbor estuary (236 km2 surface area) was investigated in previously reported drill cores (n=15) and new vibracores (n=20), reaching 3–10 m depth subsurface. Continuous vibracore facies sequences (3–4 m depth subsurface) discriminate between tidal channel and tidal flat deposition and demonstrate responses of both depositional settings to interseismic uplift and coseismic subsidence (1±0.5 m vertical) from cyclic neotectonic forcing (200–800

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26

Jensen, K. Thomas, Susana M. Ferreira, and Miguel A. Pardal. "Trematodes in a Cyathura carinata population from a temperate intertidal estuary: infection patterns and impact on host." Journal of the Marine Biological Association of the United Kingdom 84, no. 6 (2004): 1151–58. http://dx.doi.org/10.1017/s0025315404010598h.

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A study was initiated to identify trematode patterns in Cyathura from two key sites in the Mondego Estuary: a Zostera-bed and a sand flat. The two subpopulations of Cyathura differ, as the annual recruitment success is much higher and more regular on the sandflat than on the Zostera-bed.Counting and sizing of trematode cysts inside the body of preserved Cyathura specimens enabled a description of trematode patterns in space and time. Further identification of trematodes was based on DNA studies of unpreserved cysts as well as on identification of parasites in co-occurring mud snails. Two trema

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27

Zuchuat, Valentin, Arve Sleveland, Douglas Sprinkel, Algirdas Rimkus, Alvar Braathen, and Ivar Midtkandal. "New Insights on the Impact of Tidal Currents on a Low-gradient, Semi-enclosed, Epicontinental Basin—the Curtis Formation, East-central Utah, USA." Geology of the Intermountain West 5 (July 31, 2018): 131–65. http://dx.doi.org/10.31711/giw.v5.pp131-165.

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Based on a methodic sedimentological analysis, the Late Jurassic (Oxfordian) Curtis Formation unravels the intricate facies variability which occurs in a tide-dominated, fluvially starved, low-gradient, semi-enclosed epicontinental basin. This unit crops out in east-central Utah, between the eolian deposits of the underlying Middle Jurassic (Callovian) Entrada Sandstone, from which it is separated by the J-3 unconformity, and the conformable overlying supratidal Summerville Formation of Oxfordian age. A high-resolution sedimentary analysis of the succession led to the recognition of eight faci

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28

Koppel, E. M., T. L. F. Leung, and R. Poulin. "The marine limpet Notoacmea scapha acts as a transmission sink for intertidal cercariae in Otago Harbour, New Zealand." Journal of Helminthology 85, no. 2 (2010): 160–63. http://dx.doi.org/10.1017/s0022149x10000404.

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AbstractMarine limpets, Notoacmea scapha, were collected from an intertidal mud flat in Otago Harbour, New Zealand, and examined for infection with larval trematodes. Three separate species of trematode (opecoelid sp. A, Acanthoparyphium sp. A and Curtuteria australis) were identified from the limpets, based on molecular evidence. This is the first report of these three trematodes in limpets, indicating that the latter are physiologically suitable second-intermediate hosts. However, based on ecological information on the diet of the parasites' definitive hosts, we conclude that the limpet N. s

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29

Jin, Xinwei, Jingjing Fu, Juan Yang, Jing Guo, Wenrui Guo, and Yahui Chen. "Effect of Mangrove on Nitrogen Removal in the Intertidal Zone of Shenzhen’s Deep Bay: From 15N Isotope Tracing to Microbial Analysis." Water 14, no. 21 (2022): 3507. http://dx.doi.org/10.3390/w14213507.

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This study focuses on the nitrogen removal capability of the mangrove wetland system towards resolving the excessive inorganic nitrogen content in the marine water of Shenzhen’s Deep Bay. The nitrogen distribution characteristics, biological nitrogen removal processes, nitrogen removal functional genes, and bacterial community characteristics were investigated in five wetland sites in the intertidal zone of the Deep Bay, viz. the Kandelia candel, Bruguiera gymnorrhiza, Sonneratia apetala, Aegiceras corniculatum, and mud flat sites. The results showed that ammonia and nitrate in the marine wate

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30

Prosi, F., D. H. Loring, and H. Back. "Biogeochemical pathways of cadmium through an artificially contaminated intertidal mud flat system ? a medium-scale enclosure experiment." Oecologia 91, no. 3 (1992): 396–403. http://dx.doi.org/10.1007/bf00317629.

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31

Kawasaki, Kei, Akiko Sasaki-Kinoshita, and Takayuki Nakatsubo. "Annual respiration of Japanese mud snail Batillaria attramentaria in an intertidal flat: its impact on ecosystem carbon flows." Landscape and Ecological Engineering 15, no. 1 (2018): 113–20. http://dx.doi.org/10.1007/s11355-018-0365-y.

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32

Kleinhans, Maarten G., Filip Schuurman, Wiecher Bakx, and Henk Markies. "Meandering channel dynamics in highly cohesive sediment on an intertidal mud flat in the Westerschelde estuary, the Netherlands." Geomorphology 105, no. 3-4 (2009): 261–76. http://dx.doi.org/10.1016/j.geomorph.2008.10.005.

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Tanaka, Yuichi, Ayaka Horikoshi, Shigeru Aoki, and Ken Okamoto. "Experimental exclusion of the burrowing crab Macrophthalmus japonicus from an intertidal mud flat: effects on macro-infauna abundance." Plankton and Benthos Research 8, no. 2 (2013): 88–95. http://dx.doi.org/10.3800/pbr.8.88.

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34

Mussmann, Marc, Kousuke Ishii, Ralf Rabus, and Rudolf Amann. "Diversity and vertical distribution of cultured and uncultured Deltaproteobacteria in an intertidal mud flat of the Wadden Sea." Environmental Microbiology 7, no. 3 (2005): 405–18. http://dx.doi.org/10.1111/j.1462-2920.2005.00708.x.

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35

Wang, Zhanghua, Hao Xu, Qing Zhan, et al. "Lithological and Palynological Evidence of late Quaternary Depositional Environments in the Subaqueous Yangtze Delta, China." Quaternary Research 73, no. 3 (2010): 550–62. http://dx.doi.org/10.1016/j.yqres.2009.11.001.

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AMS 14C ages of post-glacial core sediments from the subaqueous Yangtze delta, along with sedimentary structures and distributions of grain size, pollen spores, and dinoflagellate cysts, show an estuarine depositional system from 13 to 8.4 cal ka BP and a deltaic system from 5.9 cal ka BP to the present. The estuarine system consists of intertidal to subtidal flat, estuarine, and estuarine-front facies, characterized by sand"mud couplets and a high sedimentation rate. The deltaic system includes nearshore shelf and prodelta mud featured by lower sedimentation rate, markedly fewer coastal wetla

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Mouritsen, Kim N., Lone T. Mouritsen, and K. Thomas Jensen. "Change of Topography and Sediment Characteristics on an Intertidal Mud-Flat Following Mass-Mortality of the Amphipod Corophium Volutator." Journal of the Marine Biological Association of the United Kingdom 78, no. 4 (1998): 1167–80. http://dx.doi.org/10.1017/s0025315400044404.

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A Corophium-bed characterized by a mosaic of emerged areas and tidal pools during low water was established on an intertidal flat in the southern part of the Danish Wadden Sea. In spring 1990, the plateaux harboured relatively high densities of the amphipod Corophium volutator, whereas the amphipods were almost absent in the pools. Following a parasite-induced mass-mortality in the population of Corophium, summer 1990, the plateaux of the bed were subjected to sediment erosion. The heterogeneous plateau-pool structure disappeared, accompanied by increased median particle diameter and decreased

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Kang, Sujin, Bohyung Choi, Yongjin Han, and Kyung-Hoon Shin. "Ecological Importance of Benthic Microalgae in the Intertidal Mud Flat of Yeongheung Island; Application of Stable Isotope Analysis (SIA)." Korean Journal of Ecology and Environment 49, no. 2 (2016): 80–88. http://dx.doi.org/10.11614/ksl.2016.49.2.080.

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38

Whomersley, P., M. Huxham, M. Schratzberger, and S. Bolam. "Differential response of meio- and macrofauna to in situ burial." Journal of the Marine Biological Association of the United Kingdom 89, no. 6 (2009): 1091–98. http://dx.doi.org/10.1017/s0025315409000344.

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Benthic nematode and macrofaunal communities are regularly utilized in impact studies. However, very few studies are carried out utilizing both communities. A literature search using the search engine Scopus (www.Scopus.com) covering the last twenty years, using the keywords ‘Macrofauna’ and ‘Disturbance’ then ‘Meiofauna’ and ‘Disturbance’ and finally ‘Macrofauna and Meiofauna’ and ‘Disturbance’, gave 210, 115 and 36 hits respectively. To assess the differential response of meio- and macrofauna to in situ burial a replicated random block designed field experiment was carried out over a 9-month

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Rowden, AA. "Sediment turnover by the stalk-eyed mud crab Hemiplax hirtipes (Brachyura: Ocypodoidea) on an intertidal flat in southeastern New Zealand." New Zealand Journal of Marine and Freshwater Research 51, no. 2 (2016): 279–94. http://dx.doi.org/10.1080/00288330.2016.1220956.

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Lee, Jun-Ho, Han Jun Woo, Hoi Soo Jung, et al. "Roles of Exposure Time and Geochemical Factors in the Characteristics of the Surface Sediments of the Hwangdo Tidal Flat, Taean, Cheonsu Bay, West Coast of Korea." Journal of Marine Science and Engineering 11, no. 9 (2023): 1697. http://dx.doi.org/10.3390/jmse11091697.

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The Hwangdo tidal flat is an intertidal landform located in Cheonsu Bay, Taean-gun, Chungcheongnam-do, on the west coast of Korea. The topographical characteristics of the semi-enclosed bay on the eastern side of the study area include waterways, sandbars, small islands, and tidal flats. In this study, data were acquired from tide gauges installed on the Hwangdo Bridge, and the height of the ellipsoid was measured using a real-time kinematics global positioning system (RTK-GPS). Digital elevation model (DEM) using Matrice 300 drone data were also acquired after processing. The geochemical sedi

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UZAKI, Ken-ichi, Fumiya YAMAZAKI, and Masahiro ABE. "DISCUSSIONS ON THE TREATMENT OF BOUNDARY CONDITIONS ON MUD WATER MOVEMENTS ON THE INTERTIDAL FLAT DUE TO SEDIMENT DISCHARGES FROM THE RIVER." Journal of Japan Society of Civil Engineers, Ser. B3 (Ocean Engineering) 78, no. 2 (2022): I_643—I_648. http://dx.doi.org/10.2208/jscejoe.78.2_i_643.

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Kerner, M. "The coupling of microbial respiration processes within the two-dimensional spatial structure of an intertidal mud flat sediment of the Elbe Estuary." SIL Proceedings, 1922-2010 24, no. 5 (1991): 3067–72. http://dx.doi.org/10.1080/03680770.1989.11899232.

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Yamamoto, Satoshi. "Geochemical study of lime-mud borings and associated coral-reef limestones in the intertidal flat of Kondoi Beach, Taketomi Island, Okinawa, Japan." Carbonates and Evaporites 17, no. 1 (2002): 44–52. http://dx.doi.org/10.1007/bf03175655.

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Brinkhoff, Thorsten, Gerard Muyzer, Carl O. Wirsen, and Jan Kuever. "Thiomicrospira kuenenii sp. nov. and Thiomicrospira frisia sp. nov., two mesophilic obligately chemolithoautotrophic sulfur-oxidizing bacteria isolated from an intertidal mud flat." International Journal of Systematic and Evolutionary Microbiology 49, no. 2 (1999): 385–92. http://dx.doi.org/10.1099/00207713-49-2-385.

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Phillips, Stephen P., John A. Howell, Adrian J. Hartley, and Magda Chmielewska. "Tidal estuarine deposits of the transgressive Naturita Formation (Dakota Sandstone): San Rafael Swell, Utah, U.S.A." Journal of Sedimentary Research 90, no. 8 (2020): 777–95. http://dx.doi.org/10.2110/jsr.2020.51.

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ABSTRACT Thin tidal estuarine deposits of the Naturita Formation (0–23 m) of the San Rafael Swell record the initial flooding of the Cretaceous Western Interior Seaway, Utah, and capture the transition from inland fluvial systems to fully marine conditions over a time period of 5 My or less. A tide-dominated estuarine environment is favored due to the combined presence of mud and/or carbonaceous drapes on ripples and dunes, bidirectional flow indicators, sigmoidal cross-stratification, herring-bone cross-stratification, and bimodal paleocurrent measurements. Facies associations are arranged in

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Kaufman, Darrell S., Steven L. Forman, Peter D. Lea, and Cameron W. Wobus. "Age of Pre-late-Wisconsin Glacial-Estuarine Sedimentation, Bristol Bay, Alaska." Quaternary Research 45, no. 1 (1996): 59–72. http://dx.doi.org/10.1006/qres.1996.0006.

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AbstractPleistocene glacial-estuarine sediment deposited in an intertidal environment of northeastern Bristol Bay, southwestern Alaska, was dated using a variety of approaches, including infrared stimulated and thermoluminescence (IRSL and TL) techniques. Analysis of modern and 14C-dated Holocene tide-flat mud demonstrates that the bulk of sediment in this environment is reset by solar radiation, thereby lending confidence to ages obtained from similar Pleistocene deposits by luminescence techniques. IRSL seems to be especially well suited for dating, with resolution on time scales of <10,0

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Mouritsen, K. N., S. McKechnie, E. Meenken, J. L. Toynbee, and R. Poulin. "Spatial heterogeneity in parasite loads in the New Zealand cockle: the importance of host condition and density." Journal of the Marine Biological Association of the United Kingdom 83, no. 2 (2003): 307–10. http://dx.doi.org/10.1017/s0025315403007124h.

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Samples of the New Zealand cockle Austrovenus stutchburyi (Veneridae) collected at two different intertidal levels were found to be heavily infected by the echinostome trematode Curtuteria australis which use the mud flat whelk Cominella glandiformis and shorebirds as first and definitive host, respectively. Parasite loads were on average more than 2-fold higher at the high site than at the low site, whereas the density of Curtuteria australis metacercariae per square metre showed the opposite trend. This pattern appeared unrelated to the abundance of first intermediate hosts and C. australis

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Abu Shady, A., Mena Fekry, M. Elsayed, Scott Durocher, and Rushdy A. Ali. "Depositional Architecture and Reservoir Quality Assessment of Abu Roash (G) Dolomite, as a Low Resistivity Pay, Razzak Oilfield, Western Desert, Egypt." Journal of Physics: Conference Series 2594, no. 1 (2023): 012004. http://dx.doi.org/10.1088/1742-6596/2594/1/012004.

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Abstract Abu-Roash (G) dolomite (A/R-G) is considered one of the most prolific oil-bearing reservoirs in the Western desert. In this study, Razzak Oilfield was selected to investigate the geological and petrophysical findings of these successions that were assigned stratigraphically to the upper Cretaceous (Late Cenomanian), in the Alamein basin. Sedimentologically, three main facies groups have been recognized in the studied successions of A/R-G and include dolostone, limestone and mudstone facies; and depositional; are divided into three parts: A) Back-reef to reef crest (Reefal depositional

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Thomas Jensen, K. "Dynamics and growth of the cockle, Cerastoderma edule, on an intertidal mud-flat in the Danish Wadden sea: Effects of submersion time and density." Netherlands Journal of Sea Research 28, no. 4 (1992): 335–45. http://dx.doi.org/10.1016/0077-7579(92)90035-d.

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Knaust, Dirk. "Ichnology as a tool in carbonate reservoir characterization: A case study from the Permian – Triassic Khuff Formation in the Middle East." GeoArabia 14, no. 3 (2009): 17–38. http://dx.doi.org/10.2113/geoarabia140317.

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ABSTRACT In the Upper Permian to Lower Triassic Khuff Formation in the Arabian Gulf, a vast shallow-marine carbonate platform developed broad facies belts with little significant changes in the lithofacies. However, trace fossil assemblages and ichnofabrics, in combination with sedimentological observations, serve in subdividing this platform and in distinguishing sub-environments. From proximal to distal, these are sabkha and salina, tidal flat, restricted lagoon, open lagoon, platform margin, shoreface/inner ramp, slope/outer ramp and basin/deeper intra-shelf. In this way, changes in relativ

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