Granier B., Feist M., Bucur I.I. & Senowbari-Daryan B. (2007).- Further investigation of the Imam's micropaleontological fraud: The stolen algae. In: Grgasović T. & Vlahović I. (eds), Field Trip Guidebook and Abstracts.- 9th International Symposium on Fossil Algae - Croatia 2007, Zagreb (September 19th-20th), Hrvatski geološki institut - Croatian Geological Survey, p. 223-224.
Algal epiphytes were examined for 12 months at Shura El-Roweysia and several tidal levels on the shore
of South Sinai dominated by Laurencia obtusa and Cystoseira myrica. Sixty seven species of the
epiphytes were recorded (41 Bacillariophyta, 20 Cyanophyta, 3 Chlorophyta and 3 Pyrrhophyta). An
inverse relationship between percentage cover of L. obtusa and their epiphytes were observed to be
affected by desiccation stress due to frequent emersion of the intertidal flat and exposure to strong
radiation, while high cover percentage of C. myrica was associated with the high number of epiphytes.
GEOLOGY OF SURINAME GOLD RUSH
https://www.researchgate.net/publication/288865395_An_explanation_to_the_geology_of_Suriname
An explanation to the geology of Suriname
October 1984
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergR.V. Van Lissa
Emond de roever
https://www.researchgate.net/publication/40160365_An_explanation_to_the_geological_map_of_Suriname
An explanation to the geological map of Suriname
January 1984
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergCissa Emond de roever
https://www.researchgate.net/publication/40160518_Igneous_and_metamorphic_complexes_of_the_GuianaShield_in_Surinam
Igneous and metamorphic complexes of the GuianaShield in Surinam
January 1983
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergK. Maas Emond de roever
https://www.youtube.com/watch?v=yJu3tat9Po4
https://www.youtube.com/watch?v=bTy87BUQyfY
https://www.facebook.com/TheMoykes/posts/10216156904223265
https://en.wikipedia.org/wiki/Suriname
https://www.vice.com/en_us/article/ppxwz9/digging-into-surinames-massive-gold-industry
This document provides an outline for a lecture on Egyptian ore deposits. It begins with an introduction discussing ancient Egyptian mining and then provides an overview of the types of mineral deposits that are known to occur in Egypt, including gold, copper, tin, zinc, lead, and various other metallic and non-metallic ores. It then discusses different classifications that have been proposed for Egyptian ore deposits, grouping them based on factors like the time of deposition, metallogenic aspects, and tectonic-magmatic stages. The document concludes by presenting a proposed classification scheme that categorizes Egyptian ore deposits into groups based on their associated rock assemblages and modes of formation.
This document provides a bibliography of references related to Sphingidae (hawkmoth) taxonomy compiled by Christophe Avon in 2016. It lists over 100 references published between 1766-2011 from sources around the world. The references cover topics such as species descriptions, distributions, host plants, and collections/museums.
This study measured nitrogen fixation through acetylene reduction by the cyanobacterium Scytonema julianum in the Vapor cave in Spain. Rates of nitrogen fixation were higher during the day than at night, likely due to energy stores being used at night. Temperature was the main factor influencing nitrogen fixation rates. Nitrogen fixation by S. julianum in the cave was roughly 30 times higher than another cave-dwelling cyanobacterium, indicating differences in environmental conditions between sites. The Vapor cave has extreme and isolated conditions including high temperatures, humidity, and carbon dioxide levels that protect S. julianum inside from external influences.
This study measured nitrogen fixation through acetylene reduction by the cyanobacterium Scytonema julianum in the Vapor cave in Spain. Rates of nitrogen fixation were higher during the day than at night, likely due to energy stores being used at night. Temperature was the main factor influencing nitrogen fixation rates. Nitrogen fixation by S. julianum in the cave was roughly 30 times higher than another cave-dwelling cyanobacterium, indicating differences in environmental conditions between sites. The Vapor cave has extreme and isolated conditions including temperatures up to 43°C and near 100% humidity that influence nitrogen cycling.
The study examines the Mn-oxide mineralization at Kato Nevrokopi, Macedonia, northern Greece using EPMA and SEM to better understand controls on formation. Todorokite, nsutite, birnessite, and chalcophanite were analyzed from different localities representing varying weathering conditions. The chemistry and textures of the Mn-oxides indicate they formed under changing pH, oxidation state, climate, and water table fluctuations during weathering. Host rock lithology and protore mineral composition also influenced the development of late-stage hypogene and early supergene Mn-oxide assemblages through controlling base metal, alkali, and alkaline earth mobilities.
Algal epiphytes were examined for 12 months at Shura El-Roweysia and several tidal levels on the shore
of South Sinai dominated by Laurencia obtusa and Cystoseira myrica. Sixty seven species of the
epiphytes were recorded (41 Bacillariophyta, 20 Cyanophyta, 3 Chlorophyta and 3 Pyrrhophyta). An
inverse relationship between percentage cover of L. obtusa and their epiphytes were observed to be
affected by desiccation stress due to frequent emersion of the intertidal flat and exposure to strong
radiation, while high cover percentage of C. myrica was associated with the high number of epiphytes.
GEOLOGY OF SURINAME GOLD RUSH
https://www.researchgate.net/publication/288865395_An_explanation_to_the_geology_of_Suriname
An explanation to the geology of Suriname
October 1984
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergR.V. Van Lissa
Emond de roever
https://www.researchgate.net/publication/40160365_An_explanation_to_the_geological_map_of_Suriname
An explanation to the geological map of Suriname
January 1984
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergCissa Emond de roever
https://www.researchgate.net/publication/40160518_Igneous_and_metamorphic_complexes_of_the_GuianaShield_in_Surinam
Igneous and metamorphic complexes of the GuianaShield in Surinam
January 1983
W. BosmaSalomon B. KroonenbergSalomon B. KroonenbergK. Maas Emond de roever
https://www.youtube.com/watch?v=yJu3tat9Po4
https://www.youtube.com/watch?v=bTy87BUQyfY
https://www.facebook.com/TheMoykes/posts/10216156904223265
https://en.wikipedia.org/wiki/Suriname
https://www.vice.com/en_us/article/ppxwz9/digging-into-surinames-massive-gold-industry
This document provides an outline for a lecture on Egyptian ore deposits. It begins with an introduction discussing ancient Egyptian mining and then provides an overview of the types of mineral deposits that are known to occur in Egypt, including gold, copper, tin, zinc, lead, and various other metallic and non-metallic ores. It then discusses different classifications that have been proposed for Egyptian ore deposits, grouping them based on factors like the time of deposition, metallogenic aspects, and tectonic-magmatic stages. The document concludes by presenting a proposed classification scheme that categorizes Egyptian ore deposits into groups based on their associated rock assemblages and modes of formation.
This document provides a bibliography of references related to Sphingidae (hawkmoth) taxonomy compiled by Christophe Avon in 2016. It lists over 100 references published between 1766-2011 from sources around the world. The references cover topics such as species descriptions, distributions, host plants, and collections/museums.
This study measured nitrogen fixation through acetylene reduction by the cyanobacterium Scytonema julianum in the Vapor cave in Spain. Rates of nitrogen fixation were higher during the day than at night, likely due to energy stores being used at night. Temperature was the main factor influencing nitrogen fixation rates. Nitrogen fixation by S. julianum in the cave was roughly 30 times higher than another cave-dwelling cyanobacterium, indicating differences in environmental conditions between sites. The Vapor cave has extreme and isolated conditions including high temperatures, humidity, and carbon dioxide levels that protect S. julianum inside from external influences.
This study measured nitrogen fixation through acetylene reduction by the cyanobacterium Scytonema julianum in the Vapor cave in Spain. Rates of nitrogen fixation were higher during the day than at night, likely due to energy stores being used at night. Temperature was the main factor influencing nitrogen fixation rates. Nitrogen fixation by S. julianum in the cave was roughly 30 times higher than another cave-dwelling cyanobacterium, indicating differences in environmental conditions between sites. The Vapor cave has extreme and isolated conditions including temperatures up to 43°C and near 100% humidity that influence nitrogen cycling.
The study examines the Mn-oxide mineralization at Kato Nevrokopi, Macedonia, northern Greece using EPMA and SEM to better understand controls on formation. Todorokite, nsutite, birnessite, and chalcophanite were analyzed from different localities representing varying weathering conditions. The chemistry and textures of the Mn-oxides indicate they formed under changing pH, oxidation state, climate, and water table fluctuations during weathering. Host rock lithology and protore mineral composition also influenced the development of late-stage hypogene and early supergene Mn-oxide assemblages through controlling base metal, alkali, and alkaline earth mobilities.
A "spare wheel" talk* on the occasion of JK2018, the International Symposium around the Jurassic - Cretaceous Boundary
*: to replace a talk of a registered speaker who could not attend the meeting
Introductory talk to JK2018, the International Symposium around the Jurassic ...Prof. Bruno R.C. Granier
Introductory talk to JK2018, the International Symposium around the Jurassic - Cretaceous Boundary (Muséum d'Histoire naturelle de Genève - CH, December 5-7, 2018)
Clues of a sedimentological model for some oolite reservoirs (example of the ...Prof. Bruno R.C. Granier
Presented on March 17, 1993, on the occasion of the Petroleum Group's meeting: "Carbonate petroleum reservoirs: Models for exploration and development"
Plea for a modern* definition of the Jurassic / Cretaceous boundary (illustr...Prof. Bruno R.C. Granier
1) The document discusses defining the boundary between the Jurassic and Cretaceous periods. Currently this boundary is placed between the Tithonian and Berriasian stages, but the author argues this is not obvious based on geological evidence.
2) The author proposes instead placing the Jurassic-Cretaceous boundary between the Berriasian and Valanginian stages. This alternative is supported by several geological events and transitions observed in the fossil and strata record.
3) The author presents geological examples and evidence from locations in Oman, Abu Dhabi, the Atlantic Ocean, and Spain to support redefining the Jurassic-Cretaceous boundary to be between the Berriasian and Valang
New data on the Hawar, Shu'aiba, Bab, and Sabsab regional stages of the Lower...Prof. Bruno R.C. Granier
Granier B., Busnardo R. & Pittet B. (2009).- New data on the Hawar, Shu'aiba, Bab, and Sabsab regional stages of the Lower Cretaceous in the United Arab Emirates and in Oman. In: Grosheny D. & Granier B. (convs.), Les corrélations plate-forme/bassin.- Volume des Résumés, École des Mines de Paris, November 30th - December 1st, p. 15-17 (abstract).
If you look for more recent publications you will find some slight changes (e.g., the TST of Shu'aiba is ascribed to the Furcata Zone of the "lower Aptian", i.e., the uppermost ammonite zone of the Bedoulian sensu gallico).
Borings and etchings in the Upper Bathonian-Lower Callovian oolite of the Par...Prof. Bruno R.C. Granier
The document discusses ooids from the Upper Bathonian-Lower Callovian formation in the Paris Basin. It found ooids with radial, concentric, and micritic fabrics that were originally calcitic. Hardgrounds and pebble layers in the succession contained borings from sponges, worms, and bivalves. Some worm borings had rough walls where early cement was less corroded than the cortices of cemented ooids, possibly due to organic matter in the cortices.
New stratigraphic data on the Lekhwair(ian) and Hawar(ian) regional stages of...Prof. Bruno R.C. Granier
1) New stratigraphic data shows that oolitic facies in Oman referred to as the "Habshan Formation" are actually of Hauterivian to Early Barremian age, and are thus part of the Lekhwair regional stage rather than correlated to the type Habshan of Abu Dhabi.
2) The Hawar interval in Oman and the UAE represents discrete third-order depositional sequences, with the Oman section showing a thin transgressive systems tract and thick highstand systems tract, reversed from the thick transgressive and thin highstand pattern in the UAE.
3) Key biostratigraphic markers like the foraminifer Choffatella help
Significance of partial leaching in calcareous ooids: The case study of Haute...Prof. Bruno R.C. Granier
Two Hauterivian oolitic units in Switzerland contain partly leached ooids. The ooids were originally calcitic, not aragonitic or two-phase. Partly leached ooid cortices do not necessarily indicate an original aragonitic mineralogy. The leaching is a late diagenetic feature possibly related to migration of acidic pore waters during Alpine tectonics and/or karstification, not early diagenesis during subaerial exposure.
A key section at L’Estellon, Drôme, France (a presentation given by Bruno R.C. Granier and coauthors on the occasion of STRATI2013). As for previous publications (Conrad et al., 2012; Charollais et al., 2013), we question the relevance of the conclusions and hypotheses of any published work based on the biased stratigraphic distribution ranges for the orbitolinids, i.e., any work based on Arnaud-Vanneau's (Arnaud-Vanneau et al., 2005, and earlier versions). There are 3 related publications: http://paleopolis.rediris.es/cg/CG2013_A03/index.html + http://paleopolis.rediris.es/cg/CG2013_A04/index.html + http://paleopolis.rediris.es/cg/CG2017_B01/CG2017_B01.pdf
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
General Data Protection Regulation (GDPR) - Training Courses - EN | PECB
Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
-------------------------------------------------------------------------------
For more information about PECB:
Website: https://pecb.com/
LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
This document provides an overview of wound healing, its functions, stages, mechanisms, factors affecting it, and complications.
A wound is a break in the integrity of the skin or tissues, which may be associated with disruption of the structure and function.
Healing is the body’s response to injury in an attempt to restore normal structure and functions.
Healing can occur in two ways: Regeneration and Repair
There are 4 phases of wound healing: hemostasis, inflammation, proliferation, and remodeling. This document also describes the mechanism of wound healing. Factors that affect healing include infection, uncontrolled diabetes, poor nutrition, age, anemia, the presence of foreign bodies, etc.
Complications of wound healing like infection, hyperpigmentation of scar, contractures, and keloid formation.
How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
How to Setup Warehouse & Location in Odoo 17 InventoryCeline George
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
How to Manage Your Lost Opportunities in Odoo 17 CRMCeline George
Odoo 17 CRM allows us to track why we lose sales opportunities with "Lost Reasons." This helps analyze our sales process and identify areas for improvement. Here's how to configure lost reasons in Odoo 17 CRM
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
A "spare wheel" talk* on the occasion of JK2018, the International Symposium around the Jurassic - Cretaceous Boundary
*: to replace a talk of a registered speaker who could not attend the meeting
Introductory talk to JK2018, the International Symposium around the Jurassic ...Prof. Bruno R.C. Granier
Introductory talk to JK2018, the International Symposium around the Jurassic - Cretaceous Boundary (Muséum d'Histoire naturelle de Genève - CH, December 5-7, 2018)
Clues of a sedimentological model for some oolite reservoirs (example of the ...Prof. Bruno R.C. Granier
Presented on March 17, 1993, on the occasion of the Petroleum Group's meeting: "Carbonate petroleum reservoirs: Models for exploration and development"
Plea for a modern* definition of the Jurassic / Cretaceous boundary (illustr...Prof. Bruno R.C. Granier
1) The document discusses defining the boundary between the Jurassic and Cretaceous periods. Currently this boundary is placed between the Tithonian and Berriasian stages, but the author argues this is not obvious based on geological evidence.
2) The author proposes instead placing the Jurassic-Cretaceous boundary between the Berriasian and Valanginian stages. This alternative is supported by several geological events and transitions observed in the fossil and strata record.
3) The author presents geological examples and evidence from locations in Oman, Abu Dhabi, the Atlantic Ocean, and Spain to support redefining the Jurassic-Cretaceous boundary to be between the Berriasian and Valang
New data on the Hawar, Shu'aiba, Bab, and Sabsab regional stages of the Lower...Prof. Bruno R.C. Granier
Granier B., Busnardo R. & Pittet B. (2009).- New data on the Hawar, Shu'aiba, Bab, and Sabsab regional stages of the Lower Cretaceous in the United Arab Emirates and in Oman. In: Grosheny D. & Granier B. (convs.), Les corrélations plate-forme/bassin.- Volume des Résumés, École des Mines de Paris, November 30th - December 1st, p. 15-17 (abstract).
If you look for more recent publications you will find some slight changes (e.g., the TST of Shu'aiba is ascribed to the Furcata Zone of the "lower Aptian", i.e., the uppermost ammonite zone of the Bedoulian sensu gallico).
Borings and etchings in the Upper Bathonian-Lower Callovian oolite of the Par...Prof. Bruno R.C. Granier
The document discusses ooids from the Upper Bathonian-Lower Callovian formation in the Paris Basin. It found ooids with radial, concentric, and micritic fabrics that were originally calcitic. Hardgrounds and pebble layers in the succession contained borings from sponges, worms, and bivalves. Some worm borings had rough walls where early cement was less corroded than the cortices of cemented ooids, possibly due to organic matter in the cortices.
New stratigraphic data on the Lekhwair(ian) and Hawar(ian) regional stages of...Prof. Bruno R.C. Granier
1) New stratigraphic data shows that oolitic facies in Oman referred to as the "Habshan Formation" are actually of Hauterivian to Early Barremian age, and are thus part of the Lekhwair regional stage rather than correlated to the type Habshan of Abu Dhabi.
2) The Hawar interval in Oman and the UAE represents discrete third-order depositional sequences, with the Oman section showing a thin transgressive systems tract and thick highstand systems tract, reversed from the thick transgressive and thin highstand pattern in the UAE.
3) Key biostratigraphic markers like the foraminifer Choffatella help
Significance of partial leaching in calcareous ooids: The case study of Haute...Prof. Bruno R.C. Granier
Two Hauterivian oolitic units in Switzerland contain partly leached ooids. The ooids were originally calcitic, not aragonitic or two-phase. Partly leached ooid cortices do not necessarily indicate an original aragonitic mineralogy. The leaching is a late diagenetic feature possibly related to migration of acidic pore waters during Alpine tectonics and/or karstification, not early diagenesis during subaerial exposure.
A key section at L’Estellon, Drôme, France (a presentation given by Bruno R.C. Granier and coauthors on the occasion of STRATI2013). As for previous publications (Conrad et al., 2012; Charollais et al., 2013), we question the relevance of the conclusions and hypotheses of any published work based on the biased stratigraphic distribution ranges for the orbitolinids, i.e., any work based on Arnaud-Vanneau's (Arnaud-Vanneau et al., 2005, and earlier versions). There are 3 related publications: http://paleopolis.rediris.es/cg/CG2013_A03/index.html + http://paleopolis.rediris.es/cg/CG2013_A04/index.html + http://paleopolis.rediris.es/cg/CG2017_B01/CG2017_B01.pdf
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
General Data Protection Regulation (GDPR) - Training Courses - EN | PECB
Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
-------------------------------------------------------------------------------
For more information about PECB:
Website: https://pecb.com/
LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
This document provides an overview of wound healing, its functions, stages, mechanisms, factors affecting it, and complications.
A wound is a break in the integrity of the skin or tissues, which may be associated with disruption of the structure and function.
Healing is the body’s response to injury in an attempt to restore normal structure and functions.
Healing can occur in two ways: Regeneration and Repair
There are 4 phases of wound healing: hemostasis, inflammation, proliferation, and remodeling. This document also describes the mechanism of wound healing. Factors that affect healing include infection, uncontrolled diabetes, poor nutrition, age, anemia, the presence of foreign bodies, etc.
Complications of wound healing like infection, hyperpigmentation of scar, contractures, and keloid formation.
How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
How to Setup Warehouse & Location in Odoo 17 InventoryCeline George
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
How to Manage Your Lost Opportunities in Odoo 17 CRMCeline George
Odoo 17 CRM allows us to track why we lose sales opportunities with "Lost Reasons." This helps analyze our sales process and identify areas for improvement. Here's how to configure lost reasons in Odoo 17 CRM
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
Walmart Business+ and Spark Good for Nonprofits.pdfTechSoup
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
Spark Good (walmart.com/sparkgood) is a charitable platform that enables nonprofits to receive donations directly from customers and associates.
Answers about how you can do more with Walmart!"
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
This slide is special for master students (MIBS & MIFB) in UUM. Also useful for readers who are interested in the topic of contemporary Islamic banking.
Leveraging Generative AI to Drive Nonprofit InnovationTechSoup
In this webinar, participants learned how to utilize Generative AI to streamline operations and elevate member engagement. Amazon Web Service experts provided a customer specific use cases and dived into low/no-code tools that are quick and easy to deploy through Amazon Web Service (AWS.)
Leveraging Generative AI to Drive Nonprofit Innovation
Further investigation of the Imam's micropaleontological fraud: The stolen algae
1. Imam,1996aImam,1996a
IMAM M.M. (1996a).- Coralline red algae from the Middle Miocene deposits of Gebel
Gushia west-central Sinai, Egypt.- Neues Jahrbuch für Geologie und Paläontologie,
Abhandlungen, 199: 1-15.
Fig. 3
2. Imam,1996aImam,1996a AGUIRRE (2004) demonstrated that
photomicrograph 3.1 labelled
“Archaeolithothamnium saipanense” was reproduced
either from JOHNSON (1957*: Pl. 37, fig. 10, where
it was called “Lithothamnium sp.”; or from his 1961:
Pl. 2, fig. 1, “Archaeolithothamnium”.
We found that JOHNSON himself re-used this photo
in 1963: Pl. 25, fig. 3, again titled
“Archaeolithothamnium”) and that it was pirated
twice more in IMAM & REFAAT (2000: Fig. 7.5) and
in IMAM (2003: Pl. 3, fig. 1).
3. Imam,1996aImam,1996a In addition, we found that
1) photomicrograph 3.7 labelled “Lithophyllum
prelichenoides” was copied, but rotated 180°, from
JOHNSON & FERRIS (1949: Pl. 38, fig. 4,
“Lithophyllum aff. prelichenoides”), or from
JOHNSON (1961: Pl. 10, fig. 3, “Lithophyllum”, or
1971: Plate 92, fig. 3, “Lithophyllum”)
JOHNSON J.H. & FERRIS B.J. (1949).-
Tertiary coralline algae from the Dutch East
Indies.- J. Pal., 23 (2): 193-198.
4. Imam,1996aImam,1996a In addition, we found that
2) photomicrograph 3.8 labelled “Jania guamensis”
was re-used from YOUSSEF et alii (1988: Fig. 14B,
“Lithophyllum sp.”) and rotated 90° clockwise when
published;
YOUSSEF E.A.A., FAHMY S.E. & IMAM M.
(1988).- Stratigraphy and microfacies of the
Miocene sequence at Gebel Sarbut El Gamal, west-
central Sinai, Egypt.- Neues Jahrbuch für Geologie
und Paläontologie, Abhandlungen, 177: 225-242.
5. Imam,1996aImam,1996a
IMAM M.M. (1996a).- Coralline red algae from the Middle Miocene deposits of Gebel
Gushia west-central Sinai, Egypt.- Neues Jahrbuch für Geologie und Paläontologie,
Abhandlungen, 199: 1-15.
Fig. 4
6. Imam,1996aImam,1996a In addition, we found that
3) photomicrograph 4.8 labelled “Lithophyllum
kladosum” was taken from Johnson (1954*: Pl. 192,
fig. 1, “Lithothamnium kladosum n. sp.”).
7. Imam,1996bImam,1996b
Imam M.M. (1996b).- Dasycladacean algae from the Turonian Wata Formation, Gebel
Um Heriba, West-Central Sinai, Egyp.- Neues Jahrbuch für Geologie und
Paläontologie, Monatshefte, 9: 527-538.
Fig. 3
8. OKLA S.M. (1992).- Further record of Jurassic, and Cretaceous fossil algae from
central Saudi Arabia.- Revue de Paléobiologie, 11 (2): 373-383.
Cylindroporella parva Pl. III, fig. 2: Salpingoporella ubaiydhi
Imam,1996bImam,1996b
9. OKLA S.M. (1991).- Dasycladacean algae from the Jurassic and Cretaceous of central
Saudi Arabia.- Micropaleontology, 37 (2): 183-190.
Cylindroporella parva Pl. 1, fig. 7: Heteroporella jaffrezoi
Imam,1996bImam,1996b
10. OKLA S.M. (1992).- Further record of Jurassic, and Cretaceous fossil algae from
central Saudi Arabia.- Revue de Paléobiologie, 11 (2): 373-383.
Heteroporella lemmensis
Pl. II, fig. 8: Dissocladella sp. (It is
more probably Cymopolia sp.)
Imam,1996bImam,1996b
11. OKLA S.M. (1991).- Dasycladacean algae from the Jurassic and Cretaceous of central
Saudi Arabia.- Micropaleontology, 37 (2): 183-190.
Heteroporella lemmensis Pl. 2, fig. 6: Salpingoporella annulata
Imam,1996bImam,1996b
12. OKLA S.M. (1991).- Dasycladacean algae from the Jurassic and Cretaceous of central
Saudi Arabia.- Micropaleontology, 37 (2): 183-190.
Salpingoporella annulata Pl. 2, fig. 7: Salpingoporella annulata
Imam,1996bImam,1996b
13. FLÜGEL E. (1979).- Paleoecology and microfacies of
Permian, Triassic and Jurassic algal communities of
platform and reef carbonates from the Alps.- Bull.
Centres Rech. Expl.-Prod. Elf-Aquitaine, 3 (2): 529-
587.
Salpingoporella milanovici
Pl. 3, fig. 4: Salpingoporella annulata (it was
re-used in STEIGER & WURM, 1980, pl. 26, fig.
2, and E. FLÜGEL, 1982, pl. 30, fig. 2)
Imam,1996bImam,1996b
14. OKLA S.M. (1992).- Further record of Jurassic, and Cretaceous fossil algae from
central Saudi Arabia.- Revue de Paléobiologie, 11 (2): 373-383.
Salpingoporella ubaiydhi Pl. III, fig. 4: Salpingoporella ubaiydhi
Imam,1996bImam,1996b
15. OKLA S.M. (1992).- Further record of Jurassic, and Cretaceous fossil algae from
central Saudi Arabia.- Revue de Paléobiologie, 11 (2): 373-383.
Trinocladus tripolitanus Pl. III, fig. 3: Salpingoporella ubaiydhi
Imam,1996bImam,1996b
16. FLÜGEL E. (1979).- Paleoecology and microfacies of Permian, Triassic and Jurassic
algal communities of platform and reef carbonates from the Alps.- Bull. Centres Rech.
Expl.-Prod. Elf-Aquitaine, 3 (2): 529-587.
Cymopolia cf. tibetica Pl. 3, fig. 5: Salpingoporella cf. pygmaea
Imam,1996bImam,1996b
17. Imam M.M. (1996b).- Dasycladacean algae from the Turonian Wata Formation, Gebel
Um Heriba, West-Central Sinai, Egyp.- Neues Jahrbuch für Geologie und
Paläontologie, Monatshefte, 9: 527-538.
Fig. 3
Okla, 1991
Okla, 1992
Flügel, 1979
Imam,1996bImam,1996b
18. Reefat&Imam,1999Reefat&Imam,1999
REFAAT A.A. & IMAM M.M. (1999).- The Tayiba Red Beds: transitional marine-
continental deposits in the precursor Suez Rift, Sinai, Egypt.- Journal of African Earth
Sciences, 28 (3): 487-506.
Fig. 9
19. GRAMBAST-FESSARD N. (1980).- Les
Charophytes du Montien de Mons (Belgique).-
Review of Palaeobotany and Palynology, 30:
67-88.
Reefat&Imam,1999Reefat&Imam,1999
Pl. IV, fig. 7 Harrisichara heteromorpha n.sp.
Pl. IV, fig. 9 Harrisichara heteromorpha n.sp.
(Holotype)
Pl. IV, fig. 8 Harrisichara heteromorpha n.sp.
Pl. IV, fig. 2 Harrisichara muricata n.sp. (Holotype)
Pl. IV, fig. 1 Harrisichara muricata n.sp.
Pl. IV, fig. 3 Harrisichara muricata n.sp.
Pl. IV, fig. 6 Harrisichara muricata n.sp. (Holotype)
20. GRAMBAST-FESSARD N. (1980).- Les
Charophytes du Montien de Mons (Belgique).-
Review of Palaeobotany and Palynology, 30:
67-88.
Reefat&Imam,1999Reefat&Imam,1999
Pl. III, fig. 2 Harrisichara regularis n.sp.
(Holotype)
Pl. III, fig. 3 Harrisichara regularis n.sp.
Pl. III, fig. 1 Harrisichara regularis n.sp.
21. GRAMBAST-FESSARD N. (1980).- Les
Charophytes du Montien de Mons (Belgique).-
Review of Palaeobotany and Palynology, 30:
67-88.
Reefat&Imam,1999Reefat&Imam,1999
Pl. II, fig. 1 Nitellopsis helicteres minor n.ssp.
(Holotype)
Pl. II, fig. 4 Nitellopsis helicteres minor n.ssp.
(Holotype)
Pl. II, fig. 2 Nitellopsis helicteres minor n.ssp.
Pl. II, fig. 3 Nitellopsis helicteres minor n.ssp.
(Holotype)
22. GRAMBAST L & GRAMBAST-FESSARD N. (1981).-
Étude sur les Charophytes tertiaires d'Europe
Occidentale. III - Le genre Gyrogona.- Paléobiologie
continentale, Montpellier, XII ( 2), 35 p.
Reefat&Imam,1999Reefat&Imam,1999
Pl. III, fig. 1 Gyrogona morelleti n.sp.
(Holotype)
23. GRAMBAST L & GRAMBAST-FESSARD N. (1981).-
Étude sur les Charophytes tertiaires d'Europe
Occidentale. III - Le genre Gyrogona.- Paléobiologie
continentale, Montpellier, XII ( 2), 35 p.
Reefat&Imam,1999Reefat&Imam,1999
Pl. I, fig. 3 Gyrogona lamarcki n.sp.
Pl. I, fig. 13 Gyrogona lemani capitata n.ssp.
(Holotype)
24. FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
Reefat&Imam,1999Reefat&Imam,1999
Pl. XII, fig. 9 Sphaerochara aff. davidi
25. Reefat&Imam,1999Reefat&Imam,1999
Pl. XIII, fig. 7 Sphaerochara aff. davidi
Pl. XIII, fig. 2 Stephanochara berdotensis n.sp.
Pl. XIII, fig. 3 Stephanochara berdotensis n.sp.
Pl. XIII, fig. 6 Stephanochara berdotensis n.sp.
FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
26. Reefat&Imam,1999Reefat&Imam,1999
REFAAT A.A. & IMAM M.M. (1999).- The Tayiba Red Beds: transitional marine-
continental deposits in the precursor Suez Rift, Sinai, Egypt.- Journal of African Earth
Sciences, 28 (3): 487-506.
Fig. 10
27. Reefat&Imam,1999Reefat&Imam,1999
Pl. I, fig. 3 Nitellopsis (Microstomella)
aptensis n.sp. (Holotype)
FEIST-CASTEL M. (1977).- Étude floristique et
biostratigraphique des Charophytes dans les séries du
Paléogène de Provence.- Géologie méditerranéenne,
Marseille, IV(2): 109-138.
28. Reefat&Imam,1999Reefat&Imam,1999
Pl. IV, fig. 1 Sphaerochara davidi n.sp. (Holotype)
Pl. IV, fig. 4 Sphaerochara davidi n.sp.
Pl. IV, fig. 7 Stephanochara oodea n.sp. (Holotype)
Pl. IV, fig. 10 Stephanochara oodea n.sp.
Pl. IV, fig. 9 Stephanochara oodea n.sp.
FEIST-CASTEL M. (1977).- Étude floristique et
biostratigraphique des Charophytes dans les séries du
Paléogène de Provence.- Géologie méditerranéenne,
Marseille, IV(2): 109-138.
29. Reefat&Imam,1999Reefat&Imam,1999
Pl. XIII, fig. 9 Rhabdochara langeri
FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
30. Reefat&Imam,1999Reefat&Imam,1999
Pl. XII, fig. 7 Chara notataFEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
31. Reefat&Imam,1999Reefat&Imam,1999
Pl. XI, fig. 3 Sphaerochara labellala n.sp.
Pl. XI, fig. 2 Sphaerochara labellala n.sp.FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
32. Reefat&Imam,1999Reefat&Imam,1999
Pl. X, fig. 10 Harrisichara subteres n.sp.
Pl. X, fig. 12 Harrisichara subteres n.sp.FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
33. GRAMBAST L & GRAMBAST-FESSARD N. (1981).-
Étude sur les Charophytes tertiaires d'Europe
Occidentale. III - Le genre Gyrogona.- Paléobiologie
continentale, Montpellier, XII ( 2), 35 p.
Reefat&Imam,1999Reefat&Imam,1999
Pl. I, fig. 2 Gyrogona lamarcki n.sp. (Paratype)
Pl. I, fig. 1 Gyrogona lamarcki n.sp. (Holotype)
Pl. I, fig. 7 Gyrogona lamarcki n.sp.
34. GRAMBAST-FESSARD N. (1980).- Les
Charophytes du Montien de Mons (Belgique).-
Review of Palaeobotany and Palynology, 30:
67-88.
Reefat&Imam,1999Reefat&Imam,1999
Pl. I, fig. 6 Dughiella ovoidea
35. Imam&reefat,2000Imam&reefat,2000
IMAM M.M. & REFAAT A.A. (2000).- Stratigraphy and facies analysis of the Miocene
sequence at Gabal Hammam Sayidna Musa and Wadi Abura, southern Sinai, Egypt.-
Neues Jahrbuch für Geologie und Paläontologie, Monatshefte, 7: 385-408.
Fig. 7
As AGUIRRE (2004) reported, in the paper of IMAM &
REFAAT (2000) dealing with Egyptian Miocene series,
“only” 2 photomicrographs (op. cit.: Fig. 7.5 and 7.6)
were pirated from JOHNSON (1961: Pl. 2, fig. 1 & Pl.
10, fig. 2) but these 2 photomicrographs and 3 others
were re-used in Imam‘s Libyan Miocene paper (2003).
As AGUIRRE (2004) reported, IMAM’s Pl. 2, fig. 6 is
Pl. 10, figs. 1 and 2 of JOHNSON (1961). He did not
mention that it had been first published as Pl. 7, fig. D of
JOHNSON & FERRIS (1950), also re-used one more
time by JOHNSON himself (1971: Plate 92, fig. 2)
36. Imam&reefat,2000Imam&reefat,2000
IMAM M.M. & REFAAT A.A. (2000).- Stratigraphy and facies analysis of the Miocene
sequence at Gabal Hammam Sayidna Musa and Wadi Abura, southern Sinai, Egypt.-
Neues Jahrbuch für Geologie und Paläontologie, Monatshefte, 7: 385-408.
Fig. 6
As Aguirre (2004) reported, in the paper of Imam &
Refaat (2000) dealing with Egyptian Miocene series,
“only” 2 photomicrographs (op. cit.: Fig. 7.5 and 7.6)
were pirated from Johnson (1961: Pl. 2, fig. 1 & Pl.
10, fig. 2) but these 2 photomicrographs and 3 others
were re-used in Imam‘s Libyan Miocene paper
(2003).
IMAM M.M. (2003).- Contribution to the stratigraphy
and paleontology of the Miocene sequence at Al Khums
area, Sirte basin, NW Libya.- Revista Española de
Micropaleontologia, 35 (2) : 195-228.
37. Imam,2000Imam,2000
Imam M.M. (2000).- On the occurence and significance of Charophyte from Ar Rajban
Member, Kiklah Formation, Wadi Ar Rajban, Mizdah Area, Northwest of Libya.-
Arab Gulf Journal of Scientific Research, Manama, vol. 18, n° 3, p. 173-183.
Plate 1
38. Imam,2000Imam,2000
Fig. 5.6 Atopochara trivolvis trivolvis
Fig. 5.5 Atopochara trivolvis trivolvis
Fig. 5.3 Atopochara trivolvis trivolvis
SOULIÉ-MÄRSCHE I. (1994).- The paleoecological
implications of the charophyte flora of the Trinity
Division, Junction, Texas.- J. Paleont., 68 (5): 1145-
1157.
39. Imam,2000Imam,2000
Pl. X, fig. 11 Rantzieniella nitida
FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
40. Imam,2000Imam,2000
Fig. 8.3 Lamphrothamnium cylindricum
Fig. 8.9 Lamphrothamnium cylindricum
Fig. 8.11 Lamphrothamnium cylindricum
Fig. 8.1 Lamphrothamnium cylindricum
SOULIÉ-MÄRSCHE I. (1994).- The paleoecological
implications of the charophyte flora of the Trinity
Division, Junction, Texas.- J. Paleont., 68 (5): 1145-
1157.
41. Imam,2000Imam,2000
Pl. XIII, fig. 1 Stephanochara berdotensis n.sp.
(Holotype)
Pl. XIII, fig. 10 Rantzieniella nitida
Pl. XIII, fig. 11 Rantzieniella nitida
Pl. XIII, fig. 5 Stephanochara berdotensis n.sp.
FEIST M. & RINGEADE M. (1977).- Étude
biostratigraphique et paléobotanique (Charophytes)
des formations continentales d’Aquitaine, de l’Éocène
supérieur au Miocène inférieur.- Bulletin de la Société
géologique de France, Paris, 7e série, XIX(2): 341-354.
42. Imam,2000Imam,2000
Pl. II, fig. 1 Musacchiella maestratica
n.sp. (Holotype)
Pl. II, fig. 4 Musacchiella maestratica
n.sp.
MARTIN-CLOSAS C. & GRAMBAST-FESSARD N.
(1986).- Les Charophytes du Crétacé inférieur de la
région du Maestrat (Chaîne Ibérique - Catalanides,
Espagne).- Paléobiologie continentale, Montpellier,
XV,:66 p..
43. Imam,2000Imam,2000
Pl. I, fig. 8 Musacchiella sp.MARTIN-CLOSAS C. & GRAMBAST-FESSARD N.
(1986).- Les Charophytes du Crétacé inférieur de la
région du Maestrat (Chaîne Ibérique - Catalanides,
Espagne).- Paléobiologie continentale, Montpellier,
XV,:66 p..
44. Imam,2000Imam,2000
Fig. 4C Musachiella douzensis n.sp.
Fig. 4B Musachiella douzensis n.sp.
FEIST M. & GRAMBAST-FESSARD N. (1984).- New
Porocharaceae from the Bathonian of Europe:
phylogeny and palaeoecology.- Palaeontology, London,
vol. 27, part 2, p. 295-305..
45. Imam,2003Imam,2003
IMAM M.M. (2003).- Contribution to the stratigraphy and paleontology of the
Miocene sequence at Al Khums area, Sirte basin, NW Libya.- Revista Española de
Micropaleontologia, 35 (2) : 195-228.
Plate 5
Aguirre (2004) made an excellent re-evaluation of the
most recent Imam publication (2003). He found that:
1) the photomicrographs of red algae in Imam‘s Pl. 5,
figs. 2 and 4 are respectively those of Pl. 10, figs. 1
and 2 of Johnson (1961). He did not mention that
both of these illustrations had been first published,
respectively as Pl. 6, fig. D and Pl. 7, fig. D of Johnson
& Ferris (1950), also re-used one more time by
Johnson himself (1971: Plate 92, figs. 1 and 2).
2) Imam‘s Pl. 5, fig. 9 corresponds to Pl. 26, fig. 3 of
Johnson (1963). He did not mention that Johnson
(1961) had reproduced it from Pl. IX, fig. 2 of
Pfender (1926).
Johnson & Ferris, 1950
Pfender, 1926
Piller & Rasser, 1997
Aguirre et alii, 1993
Martin et alii, 1997
Martin et alii, 1993
46. Imam,2003Imam,2003
IMAM M.M. (2003).- Contribution to the stratigraphy and paleontology of the
Miocene sequence at Al Khums area, Sirte basin, NW Libya.- Revista Española de
Micropaleontologia, 35 (2) : 195-228.
Plate 3
johnson, 1957
Imam & Refaat, 2000
Aguirre et alii, 1993
johnson, 1964
47. Imam,2003Imam,2003
IMAM M.M. (2003).- Contribution to the stratigraphy and paleontology of the
Miocene sequence at Al Khums area, Sirte basin, NW Libya.- Revista Española de
Micropaleontologia, 35 (2) : 195-228.
Plate 4
Martin et alii, 1997
Imam & Refaat, 2000
johnson & Steward, 1953
Martin & Braga, 1993
48. References:
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France, Paris, 7e
série, XIX(2): 341-354.
Feist M. & Grambast-Fessard N. (1984).- New Porocharaceae from the Bathonian of Europe: phylogeny and
palaeoecology.- Palaeontology, London, 27(2): 295-305.
Feist-Castel M. (1977).- Étude floristique et biostratigraphique des Charophytes dans les séries du Paléogène de
Provence.- Géologie méditerranéenne, Marseille, IV(2): 109-138.
Flügel E. (1979).- Paleoecology and microfacies of Permian, Triassic and Jurassic algal communities of platform
and reef carbonates from the Alps.- Bull. Centres Rech. Expl.-Prod. elf aquitaine, Pau, 3 (2): 529-587.
Grambast-Fessard N. (1980).- Les Charophytes du Montien de Mons (Belgique).- Review of Palaeobotany and
Palynology, 30: 67-88.
Grambast L & Grambast-Fessard N. (1981).- Étude sur les Charophytes tertiaires d'Europe Occidentale. III - Le
genre Gyrogona.- Paléobiologie continentale, Montpellier, XII(2): 35 p.
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Egypt.- Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 199: 1-15.
Imam M.M. (1996b).- Dasycladacean algae from the Turonian Wata Formation, Gebel Um Heriba, West-Central
Sinai, Egyp.- Neues Jahrbuch für Geologie und Paläontologie, Monatshefte, 9: 527-538.
Imam M.M. (2000).- On the occurence and significance of Charophyte from Ar Rajban Member, Kiklah
Formation, Wadi Ar Rajban, Mizdah Area, Northwest of Libya.- Arab Gulf Journal of Scientific Research.,
Manama, 18(3): 173-183.
Imam M.M. (2003).- Contribution to the stratigraphy and paleontology of the Miocene sequence at Al Khums
area, Sirte basin, NW Libya.- Rev. Españ. Micropal., 35 (2) : 195-228.
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Monatshefte, 7: 385-408.
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Okla S.M. (1991).- Dasycladacean algae from the Jurassic and Cretaceous of central Saudi Arabia.-
Micropaleontology, 37(2): 183-190.
Okla S.M. (1992).- Further record of Jurassic, and Cretaceous fossil algae from central Saudi Arabia.- Rev.
Paléobiol., Genève, 11(2): 373-383.
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Paris, (2), III( 6):1-32.
Refaat A.A. & Imam M.M. (1999).- The Tayiba Red Beds: transitional marine-continental deposits in the
precursor Suez Rift, Sinai, Egypt.- J. Afric. Earth Sci., 28 (3): 487-506.
Soulié-Märsche I. (1994).- The paleoecological implications of the charophyte flora of the Trinity Division,
Junction, Texas.- J. Paleont., 68 (5): 1145-1157.