Skip to main content Accessibility help
×
Hostname: page-component-68945f75b7-z8dg2 Total loading time: 0 Render date: 2024-08-05T16:10:04.331Z Has data issue: false hasContentIssue false

Introduction

Published online by Cambridge University Press:  27 April 2010

Roger V. Jean
Affiliation:
Université du Québec, Montréal
Get access

Summary

Introduction

In addition to the descriptive aspects of phyllotaxis (Part I), there are more fundamental matters concerned with the causes inducing phyllotactic patterns. How do plants achieve such pattern formation, especially when sometimes apparently quite extraordinary precision is attained, as we have seen? Where does the control come from that establishes the beautiful natural patterns described here? There are several hypotheses and mathematical models designed to explain the dynamical and causal aspects of pattern formation in phyllotaxis. The main hypotheses and/or models can be roughly categorized as:

1. Physical. Snow and Snow's first available space hypothesis (1962) that predicts the formation of a new primordium, whenever by growth a certain minimal amount of space becomes available at the apex. Esau's (1965b) and Larson's (1977) procambial strands hypothesis insisting on the acropetal influence of the vascular traces in the determination of leaves and in pattern formation. Plantefol's (1948,1950) hypothesis (see Section 2.6) which calls upon Snow and Snow's in order to explain some observations. Schwendener's (1878) hypothesis and Adler's (1977a) model that base pattern formation on mutual physical contact pressures between primordia. Green's reinforcement patterns of cells (1985) and bulging phenomenology of the tunica (1992), for which patterns are the results of surface stresses between cells.

Type
Chapter
Information
Phyllotaxis
A Systemic Study in Plant Morphogenesis
, pp. 123 - 126
Publisher: Cambridge University Press
Print publication year: 1994

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

  • Introduction
  • Roger V. Jean, Université du Québec, Montréal
  • Book: Phyllotaxis
  • Online publication: 27 April 2010
  • Chapter DOI: https://doi.org/10.1017/CBO9780511666933.009
Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

  • Introduction
  • Roger V. Jean, Université du Québec, Montréal
  • Book: Phyllotaxis
  • Online publication: 27 April 2010
  • Chapter DOI: https://doi.org/10.1017/CBO9780511666933.009
Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

  • Introduction
  • Roger V. Jean, Université du Québec, Montréal
  • Book: Phyllotaxis
  • Online publication: 27 April 2010
  • Chapter DOI: https://doi.org/10.1017/CBO9780511666933.009
Available formats
×