Bilal Haq | |
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Born | Bilal Ul Haq 8 October 1948 |
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Scientific career | |
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Punjab]] |
Thesis | Paleogene Calcareous Nannoflora: Rates of Evolution in Cenozoic Calcareous Nannoplankton (1972) |
Doctoral advisor | Ivar Hessland |
Website |
Bilal U. Haq is a Pakistani-American geoscientist (and poet) who is currently affiliated with and divides his time between the Smithsonian Institution in Washington, DC, and Sorbonne University's Institute of Earth Sciences in Paris, France. He is best known for his work on the Phanerozoic sea-level fluctuations and eustatic curves that are widely used in the academia and industry as the basis for global stratigraphy and in exploration geology. He is a laureate of the Prestwich Prize for geosciences from France.
Bilal Haq was born in the foothills of Himalayas (Gorakhpur) where his father Mohammad Fazl-i-Haq was a senior ICS officer in the British Indian government. After the independence of India his father opted to serve in the new nation of Pakistan since his family originated from Lahore, now in Pakistan. He received his early education at St. Paul's and Central Model Schools in Karachi and Lahore, respectively. In Lahore, he also earned his Bachelor and Master of Science degrees from the Government College and the Punjab University. In Europe, after receiving a diploma in German language from Dolmetscher Institut of Heidelberg University, he started his graduate research at the University of Vienna [1] and then moved to Sweden to earn his PhD and DSc degrees in marine geoscience from the University of Stockholm. [2]
Bilal U. Haq's career spans over five decades, and he has carried out research in several disciplines of marine geosciences at the University of Stockholm, the Woods Hole Oceanographic Institution in Massachusetts, [3] Exxon Production Research Company in Houston, [4] the National Science Foundation in Washington, DC, [5] the Universities of Copenhagen, [6] Cambridge, Oxford, [7] Paris (UPMC, [8] Sorbonne [9] ) and Utrecht. He has consulted with, provided advice to, or delivered specialized courses to numerous multinational resource companies, and geological surveys around the world through his consulting partnership. [10]
He was seconded to the World Bank in Washington, DC in their Environment Department, where already in 1994 he produced a special report on the effects of climate change and sea-level rise on the economies of developing maritime nations. [11] [12]
In 1994, Bilal was also seconded by NSF to the White House's Executive Office of the US president for the Federal Budget where he worked on the science budget for independent science agencies. [13] Bilal was appointed an honorary professor at both Tongji University in Shanghai and the Academia Sinica Institute of Ocean Sciences in Qingdao, China, and was a visiting professor at both Oxford and Cambridge Universities in the UK.
Bilal Haq is also a poet who has published four volumes of poetry, [14] with insights into nature and the nature of man. His poetic license, enabled by his scientific background, has been fondly dubbed by his peers as "geopoetry", and his poetic message is that we have to learn to live with nature, if we are to survive.
Among Bilal's many services to the scientific community was his rescue of a prolific fossil site in the Shandong province of China (Confucius' birthplace) through an international appeal, [15] (now a National Geopark). He also conceived and helped create a paleontological Geopark (together with the Chinese biologist and academician, Zheng Shouyi) consisting of giant sculptures based on fossil micro-organisms (Foraminifera) in Zhongshan City in Guangdong Province. [16] [17] Since its opening in December 2009, the sculpture park has been visited by over 200,000 visitors every year, which the Smithsonian magazine declared the second most important "Evo-tourism" site in the world. [18] This was followed by another, larger, Foraminiferal sculpture park in the city of Qingdao, that was established in 2017.
Bilal Haq's research covers a broad spectrum of geosciences, from marine geology to marine sedimentology, paleoceanography, paleoclimatology, paleobiogeography, biostratigraphy, seismic, sequence and global stratigraphy, and natural gas hydrates. In the past his focus was on documenting sea-level changes along the world's continental margins and interior basins for the last 550 million years of Earth history (the complete Phanerozoic Eon). [19] [20] [21] [22] [23] More recently he has directed his attention to influence of tectonics on the sedimentary record. [24] [25] He has also focused on quantifying the amount of total Messinian salt sequestered in the deep Mediterranean evaporite giant and its implications for tectonics in various deep basins and continental margins and the paleoceanography of this enclosed Sea. [26] Bilal has published over 160 research papers, book chapters and encyclopedia articles, several of them among the most highly cited in Earth sciences, [27] of which one was chosen as among the top 100 papers in geosciences of all time. [28]
Bilal Haq's honors include the Shepard Medal for excellence in marine geology, [29] [30] the Ocean Sciences Award from the American Geophysical Union, [31] the Antarctic Medal of the US National Science Foundation, and more recently the Prestwich Prize [32] [33] from the Geological Society of France. The Geological Society of America recently recognized his contributions to geosciences with their International Distinguished Career Award. He has also been recognized for his research by the award of a doctoris honoris causa by the Sorbonne University, election to the membership of the European Academy of Science and Letters (Academia Europaea), [34] and to fellowships of the American Association for the Advancement of Science and the Geological Society of America. Bilal has also been honored by his peers with the naming of a fossil plankton species and a genus after him. His international appeal saved a prolific fossil site from destruction (that was later declared a National Geopark) in Shandong Province in China and he helped create two Foraminiferal sculpture parks in Guangzhou and Qingdao.
Bilal Haq has published four volumes of poetry: Reflections (2016), Musings (2017), Ruminations (2017) and Glimpses of Nature and Man (2018). [14]
The Cambrian is the first geological period of the Paleozoic Era, and the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran period 538.8 Ma to the beginning of the Ordovician Period 485.4 Ma.
An extinction event is a widespread and rapid decrease in the biodiversity on Earth. Such an event is identified by a sharp fall in the diversity and abundance of multicellular organisms. It occurs when the rate of extinction increases with respect to the background extinction rate and the rate of speciation. Estimates of the number of major mass extinctions in the last 540 million years range from as few as five to more than twenty. These differences stem from disagreement as to what constitutes a "major" extinction event, and the data chosen to measure past diversity.
The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at 443.8 million years ago (Mya), to the beginning of the Devonian Period, 419.2 Mya. The Silurian is the third and shortest period of the Paleozoic Era, and the third of twelve periods of the Phanerozoic Eon. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out.
The Triassic is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic.
The Archean Eon, in older sources sometimes called the Archaeozoic, is the second of the four geologic eons of Earth's history, preceded by the Hadean Eon and followed by the Proterozoic. The Archean represents the time period from 4,031 to 2,500 Mya. The Late Heavy Bombardment is hypothesized to overlap with the beginning of the Archean. The Huronian glaciation occurred at the end of the eon.
Foraminifera are single-celled organisms, members of a phylum or class of Rhizarian protists characterized by streaming granular ectoplasm for catching food and other uses; and commonly an external shell of diverse forms and materials. Tests of chitin are believed to be the most primitive type. Most foraminifera are marine, the majority of which live on or within the seafloor sediment, while a smaller number float in the water column at various depths, which belong to the suborder Globigerinina. Fewer are known from freshwater or brackish conditions, and some very few (nonaquatic) soil species have been identified through molecular analysis of small subunit ribosomal DNA.
The Cryogenian is a geologic period that lasted from 720 to 635 million years ago. It is the second of the three periods of the Neoproterozoic era, preceded by the Tonian and followed by the Ediacaran.
The Ediacaranbiota is a taxonomic period classification that consists of all life forms that were present on Earth during the Ediacaran Period. These were enigmatic tubular and frond-shaped, mostly sessile, organisms. Trace fossils of these organisms have been found worldwide, and represent the earliest known complex multicellular organisms. The term "Ediacara biota" has received criticism from some scientists due to its alleged inconsistency, arbitrary exclusion of certain fossils, and inability to be precisely defined.
The geology of China consists of three Precambrian cratons surrounded by a number of orogenic belts. The modern tectonic environment is dominated by the continued collision of India with the rest of Asia starting 40–50 million years ago. This has formed the Himalayas and continues to deform most of China. China has vast mineral reserves, a significant earthquake risk in its western regions and rare isolated active volcanoes throughout the country.
Government Central Model School, Lahore is a public school in Lahore, Punjab, Pakistan. More than 3,000 students study in the school.
The Institute of Geosciences is a unit of instruction of the Federal University of Rio Grande do Sul (UFRGS). It includes the undergraduate courses of Geography, Geomatics Engineering, Geology. It has a department of study of vertebrate paleontology which has made great contributions to the geopark of Paleorrota.
Wolfgang "Wolf" Helmut Berger was a German-American oceanographer, geologist, micropaleontologist and emeritus professor at Scripps Institution of Oceanography and the University of California, San Diego. His research interests comprise "micropaleontology, marine sedimentation, ocean productivity, carbon cycle, ocean history, climate history, and history of oceanography."
The Washington Formation is a coal, sandstone, and limestone geologic formation located in Ohio, Pennsylvania and West Virginia. It dates back to the Lower Permian period, with its base at or near the Permian/Carboniferous boundary. The Washington formation and the Dunkard Group as a whole was deposited at a time when the continents were in the process of forming the "Super Continent" Pangaea as well as a gradual drop in sea levels. The result during this period was coals being thinner and impure with high ash content. The limestones found with in the formation are exclusively freshwater deposits.
The Cretaceous–Paleogene (K–Pg) extinction event, also known as the K–T extinction, was the mass extinction of three-quarters of the plant and animal species on Earth approximately 66 million years ago. The event caused the extinction of all non-avian dinosaurs. Most other tetrapods weighing more than 25 kg (55 lb) also became extinct, with the exception of some ectothermic species such as sea turtles and crocodilians. It marked the end of the Cretaceous period, and with it the Mesozoic era, while heralding the beginning of the current era, the Cenozoic. In the geologic record, the K–Pg event is marked by a thin layer of sediment called the K–Pg boundary, Fatkito boundary or K–T boundary, which can be found throughout the world in marine and terrestrial rocks. The boundary clay shows unusually high levels of the metal iridium, which is more common in asteroids than in the Earth's crust.
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