Skip to main content
Top

2018 | OriginalPaper | Chapter

2. Why Did Life Generate? Why Does Life Evolve? Physical Perspective of the Origin of Life

Author : Hiromoto Nakazawa

Published in: Darwinian Evolution of Molecules

Publisher: Springer Singapore

Activate our intelligent search to find suitable subject content or patents.

search-config
loading …

Abstract

To approach the origin of life, the physical inevitability of generation and evolution of life is the fundamental issue that must be first addressed. The question “Why did life generate?” asks essentially the same question as “Why does life evolve?” since it demands a physical reason for the organization of organic molecules to higher complexity in the dynamic environment on Earth. As reviewed in Chapter 1, Earth has been radiating heat to space for the 4.6 billion years since its formation. This indicates from the view of the second law of thermodynamics that the decrease of Earth’s entropy due to radiation of heat is the cause of life’s instigation and its evolution to the present biodiversity.

Dont have a licence yet? Then find out more about our products and how to get one now:

Springer Professional "Wirtschaft+Technik"

Online-Abonnement

Mit Springer Professional "Wirtschaft+Technik" erhalten Sie Zugriff auf:

  • über 102.000 Bücher
  • über 537 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Finance + Banking
  • Management + Führung
  • Marketing + Vertrieb
  • Maschinenbau + Werkstoffe
  • Versicherung + Risiko

Jetzt Wissensvorsprung sichern!

Springer Professional "Technik"

Online-Abonnement

Mit Springer Professional "Technik" erhalten Sie Zugriff auf:

  • über 67.000 Bücher
  • über 390 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Maschinenbau + Werkstoffe




 

Jetzt Wissensvorsprung sichern!

Footnotes
1
When a high-temperature object (T1) is placed in contact with a low-temperature object (T2), heat flows from the high-temperature object to the low-temperature object, until both objects reach the same temperature. If heat flow is ∆Q, the entropy of the low-temperature object increases ∆Q/T2 while that of the high-temperature object decreases ∆Q/T1. The total entropy change ∆S of this “universe,” i.e., the total entropy change of an isolated system is defined as ∆S = ∆Q/T2 −∆Q/T1. Since T2 < T1, the total entropy change (∆S) of the isolated system (“the universe”) is always positive; i.e., it increases during heat flow from a high-temperature object to a low-temperature object.
 
2
Entropy (S) is given by the expression S = klogW, where k is the Boltzmann constant, k = 1.3806488 × 1023 J/K, and W is the number of states of microparticles. Since the unit of k is J/K, “the amount of heat (Joule)/temperature (K),” it is also involved in macroscopic quantities, such as temperature, heat, and specific heat. Therefore, k is an important constant that connects the macroscopic and micro-particulate realms. The epitaph on the tomb of L. Boltzmann in Vienna, Austria, reads simply “S = klogW” in concise recognition of his most significant achievement.
 
Literature
go back to reference Anglada-Escude G, Amado PJ, Barnes J, Berdinas ZM, Butler RP, Coleman GA., de la Cueva I, Dreizler S, Endl M, Giesers B, Jeffers SV, Jenkins JS, Jones HRA, Kiraga M, Kürster M, Lopez-Gonzalez MJ, Marvin CJ, Morales N, Morin J, Nelson RP, Ortiz JL, Ofir A, Paardekooper S, Reiners A, Rodrigues E, Rodrigues-Lopez C, Samiernto LF, Strachan JP, Tsapras Y, Sechneiuster TM (2016) A terrestrial planet candidate in a template orbit around Proxima Centaui, Nature 536:437–440CrossRef Anglada-Escude G, Amado PJ, Barnes J, Berdinas ZM, Butler RP, Coleman GA., de la Cueva I, Dreizler S, Endl M, Giesers B, Jeffers SV, Jenkins JS, Jones HRA, Kiraga M, Kürster M, Lopez-Gonzalez MJ, Marvin CJ, Morales N, Morin J, Nelson RP, Ortiz JL, Ofir A, Paardekooper S, Reiners A, Rodrigues E, Rodrigues-Lopez C, Samiernto LF, Strachan JP, Tsapras Y, Sechneiuster TM (2016) A terrestrial planet candidate in a template orbit around Proxima Centaui, Nature 536:437–440CrossRef
go back to reference Ida S (2003) Variant of the planet, from a formation theory of extrasolar planet (in Japanese). NHK Books, Tokyo, p 227 Ida S (2003) Variant of the planet, from a formation theory of extrasolar planet (in Japanese). NHK Books, Tokyo, p 227
go back to reference Ijiri S (1968) Kaseki (in Japanese, Fossils), Iwanami-Shinsho vol 673. Tokyo, pp 66–79 Ijiri S (1968) Kaseki (in Japanese, Fossils), Iwanami-Shinsho vol 673. Tokyo, pp 66–79
go back to reference Nomura R, Hirose K, Uesugi K, Ohishi Y, Tsuchiyama A, Miyake A, Ueno Y (2014) Low core-mantle boundary temperature inferred from the solidus of pyrolite. Science 343:522–525CrossRef Nomura R, Hirose K, Uesugi K, Ohishi Y, Tsuchiyama A, Miyake A, Ueno Y (2014) Low core-mantle boundary temperature inferred from the solidus of pyrolite. Science 343:522–525CrossRef
go back to reference Schrödinger E (1944) What is life?—The physical aspect of the living cell. Cambridge University Press, London Schrödinger E (1944) What is life?—The physical aspect of the living cell. Cambridge University Press, London
go back to reference Tajika E (1996) The Chapter 2, Construction of the earth, in Introduction to Earth and planetary science (in Japanese). Iwanamishoten, Tokyo, pp 92 and 96 Tajika E (1996) The Chapter 2, Construction of the earth, in Introduction to Earth and planetary science (in Japanese). Iwanamishoten, Tokyo, pp 92 and 96
go back to reference The KamLAND Collaboration (2011) Partial radiogenic heat model for Earth revealed by geonutrino measurements. Nat Geosci 4:647–651. Online Publication 17 July 2011 The KamLAND Collaboration (2011) Partial radiogenic heat model for Earth revealed by geonutrino measurements. Nat Geosci 4:647–651. Online Publication 17 July 2011
Metadata
Title
Why Did Life Generate? Why Does Life Evolve? Physical Perspective of the Origin of Life
Author
Hiromoto Nakazawa
Copyright Year
2018
Publisher
Springer Singapore
DOI
https://doi.org/10.1007/978-981-10-8724-0_2