For a commented initial example, see: e. Coli K-12 MG1655 gene thrA.

KEGG does the visual maps well.

But BioCyc is generally better otherwise.

Present at: www.roche.com/about/philanthropy/science-education/biochemical-pathways/

TODO human presumably?

I don't think it has any advantage over KEGG however, besides historical interest? Maybe slightly more manual layout and so more beautiful?

James Somers (rightly) likes to point to it as a "biology is awesome" thing.

An artificial metabolic pathway using synthetic biology technology.

Design software for synthetic biological circuit.

The input is in Verilog! Overkill?

Then it essentially maps to a standard cell library of biological primitives!

You label cells with isotopes rather than fluorescent substances. Vendors claim that this allows much wider N-way sorts, e.g. 2022 Fluidigm claims around 40/50, because the fluorecent spectrum is too wide to do much more than 7/8 way splits.

A photocathode is a type of material that emits electrons when it absorbs light, a process known as the photoelectric effect. It typically consists of a semiconductor or a metal that is sensitive to particular wavelengths of light. When photons strike the surface of the photocathode, they can impart enough energy to the electrons within the material to overcome the work function (the minimum energy needed for an electron to escape from the surface).

Yttria-stabilized zirconia (YSZ) is a crystalline compound formed by the addition of yttrium oxide (Y2O3) to zirconium dioxide (ZrO2). This stabilization process is essential because zirconia can exist in different crystalline forms (phases), and at high temperatures, it can transform from its stable monoclinic form to a tetragonal or cubic form. However, this phase transformation can make pure zirconia brittle.

The Balleny hotspot is a geologically significant area located in the southern Indian Ocean, primarily associated with the Balleny Islands and the broader region. It is characterized by volcanic activity and is considered a hotspot due to its anomalous geological features, including the formation of undersea volcanic islands and seamounts as a result of mantle plume activity. Hotspots are typically regions where hot mantle material rises and creates volcanic activity independently of tectonic plate boundaries.

The Bellona Platform is a decentralized ecosystem designed to facilitate the integration and use of various blockchain technologies and digital assets. It aims to provide a user-friendly interface for developers and users to access a range of blockchain services, including decentralized applications (dApps), smart contracts, and digital asset management. Some key features of the Bellona Platform may include: 1. **Interoperability**: The platform often focuses on enabling seamless interactions between different blockchain networks to enhance functionality and expand user capabilities.

The Caledonian Ocean, also known as the Caledonian Sea, refers to a prehistoric ocean that existed during the Paleozoic Era, particularly during the Silurian and early Devonian periods, around 440 to 360 million years ago. It was situated between the continents of Laurentia (which is now part of North America and Greenland) and Baltica (which included parts of modern-day Europe and Scandinavia).

Campi Flegrei, also known as the Phlegraean Fields, is a large volcanic area located near Naples, Italy, not in Sicily. It is known for its calderas, fumaroles, and a history of explosive volcanic activity, including a major eruption around 39,000 years ago that significantly affected the climate and environment of the region.

Davidson Current, also known as the Davidson Channel Current, is a significant oceanic flow found in the Southern Ocean, particularly around the Antarctic region. This current is named after the Davidson Channel, which is located between the South Shetland Islands and the Antarctic Peninsula. The Davidson Current is characterized by its relatively shallow depth and its influence on local marine environments, including the distribution of nutrients, sea ice, and marine life.

The Eurasian Basin is a significant geological and geographical region located in the Arctic Ocean. It is part of the broader Arctic region and is characterized by its relatively shallow waters compared to other ocean basins. Here are some key features of the Eurasian Basin: 1. **Geographical Location**: The Eurasian Basin is bordered by the continents of Europe and Asia to the south, while the North Pole lies to the north.

The Guinea Current is an ocean current that flows along the coast of West Africa, particularly off the coast of Guinea. It is part of the North Atlantic Ocean circulation and is influenced by various factors, including the winds, the configuration of the coastline, and the temperature and salinity of the water. The Guinea Current generally moves in a westward direction, originating from the equatorial region, and it is a significant component of the Atlantic Meridional Overturning Circulation.

Hall Basin refers to a specific geological feature located in Antarctica, particularly in the eastern section of the continent. It is a subglacial basin, meaning it is situated beneath ice sheets, and is primarily filled with glacial ice. The basin has been of interest to scientists due to its potential implications for understanding ice sheet dynamics and contributions to sea-level rise. The studies in Hall Basin focus on various aspects such as subglacial hydrology, geology, and the history of ice flow in the region.

Heck Seamount is an underwater volcanic feature located in the Pacific Ocean, specifically to the southeast of the Hawaiian Islands. It is part of the Hawaiian-Emperor seamount chain, which is a series of underwater mountains formed by volcanic activity. Seamounts like Heck are typically associated with hotspot volcanism, where tectonic plate movement over a stationary mantle plume creates volcanic features.

The Hofmann Trough, also known as the Hofmann type trough, is a specialized piece of equipment used primarily in chemical laboratories for conducting experiments involving the behavior of liquids and gases. It is named after the chemist August Wilhelm von Hofmann. This trough is usually designed to allow for the observation of phenomena such as surface tension, capillarity, or the interaction of different liquid phases.

Kane Basin is a body of water located between Greenland and the Arctic archipelago of Canada. Specifically, it is situated between the northeastern coast of Greenland and the southwestern shore of Ellesmere Island, which is part of Canada. Kane Basin is known for its cold Arctic waters and is part of the larger Nares Strait, which connects Baffin Bay in the west to the Arctic Ocean in the east.