The characters of lotus stomatal development

 

 

A Review on the Taxonomic, Evolutionary and Phytogeographic Studies of the Lotus Plant (Nelumbonaceae: Nelumbo)

by Li Y., Popova S., Yao J., Li C. (2014)

Ya Li

Ningbo Institute of Materials Technology and Engineering (Ningbo, China)

Svetlana_Popova5
Svetlana Popova, Russian Academy of Sciences, Moscow, Russia

Jianxin Yao

Chinese Academy of Geological Sciences (Beijing, China)

Chengsen Li, Chinese Academy of Sciences (Beijing, China) 

in Acta Geologica Sinica 88(4) – DOI: 10.1111/1755-6724.12287 –

https://www.researchgate.net/publication/265912612_A_Review_on_the_Taxonomic_Evolutionary_and_Phytogeographic_Studies_of_the_Lotus_Plant_Nelumbonaceae_Nelumbo

Abstract
Nelumbo Adans. (Nelumbonaceae) is an important member of the early-diverging eudicots. It contains two extant species: N. nucifera Gaertn. (the Sacred lotus), distributed in Asia and Australia and N. lutea Willd. (the American lotus), occurring in North America.
This paper reviews the taxonomic, evolutionary and phytogeographic studies of the genus Nelumbo, and also raises scientific questions about it in further paleobotanic research.
There are about 30 fossil species of Nelumbo established since the Early Cretaceous. Based on fossil studies, the ancestors of the extant N. nucifera and N. lutea are respectively considered to be N. protospeciosa from the Eocene to Miocene of Eurasia, and N. protolutea from the Eocene of North American. However, molecular systematic studies indicate that N. nucifera and N. lutea are probably split from a common ancestor during the Late Miocene to Early Pliocene, or even the Pleistocene, rather than separate relicts from extinct species on different continents.
The characters of lotus stomatal development, seedling morphology as well as its flowering, pollination and fertilization in air reveal that it evolves from the land plants. Fossil data of Nelumbo indicates that the genus first occurs in mid-latitude area of Laurasia in the Early Cretaceous, then becomes widespread in North America and Eurasia and expands into Africa and South America during the Late Cretaceous; the genus probably colonizes the Indian Subcontinent from Asia during the Early Eocene after the collision of India and the Asian plates; the genus becomes extinct in Europe, but survives in Asia and North America during the Quaternary Ice Age, and later forms the present East Asia and North Australia-North America disjunctive distribution.
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Stomata in fossil land plants of 445 million years ago

Screen Shot 2018-03-23 at 18.31.14
A reconstruction of Cooksonia, one of the earliest known land plants. Photograph: Matteo De Stefano/MUSE via Wikimedia Commons

 

How the earliest plants made our world muddy

The first plants to make it on to land altered mud production and where it formed rocks, changing our planet forever

by Lydon S. (2018)

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in The Guardian 2018-03-23 –

https://www.theguardian.com/science/2018/mar/23/how-the-earliest-plants-made-our-world-muddy

How and when the earliest plants made the first move on to land is always a hot topic for palaeobotanists. We know that early land plants likely evolved from freshwater algae, gaining a bunch of necessary adaptations in the process. Plants needed to support themselves, protect themselves from drying out and from the harmful effects of UV light, and gain water and nutrients from a finite supply on land. A study published last week by Mariusz Salamon and colleagues described fossils that push back the earliest evidence of land plants to around 445 million years ago.

The new fossils come from mudstones in central Poland, in beds that have been dated using other, much more common and cosmopolitan, fossils. The plant remains are tiny, branched fragments, up to about 3mm long. Some specimens appear to have spore-cases at the top of their branches, similar to those seen in younger, better-known early land plants such as Cooksonia. The preservation of the plants means details are hard to discern, but Salamon and colleagues present a single, tantalising stoma, or air pore, on one of the fragments as a key piece of evidence. If this plant had stomata for gas exchange, it was likely to have been living in land, a good 15 million years earlier than previously known plant fragments.


 

 

 

Leaf epidermal cells of “living fossil” species are more sensitive than stomata to a doubling of CO2 concentration.

Screen Shot 2018-02-07 at 19.51.15
Fig. 1. Detail of a microscope observation of stomata and epidermal cells in a Sequoia sempervirens leaf abaxial surface.

 

Density and length of stomatal and epidermal cells in “living fossil” trees grown under elevated CO2 and a polar light regime

by Ogaya R., Llorens L., Penuelas (2011)

R. Ogaya a,*, L. Llorens b,1 , J. Peñuelas a

a Global Ecology Unit CREAF-CEAB-CSIC, CREAF (Center for Ecological Research and Forestry Applications), Universitat Autònoma de Barcelona, 08193 Bellaterra, Barcelona, Spain

b Department of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK

=======

in Acta Oecologica 37: 381-385 –

http://www.creaf.uab.es/global-ecology/Pdfs_UEG/2011%20ActaOecol.pdf

Abstract

During the Cretaceous and early Tertiary, when the climate was warm and the atmospheric CO2 concentration ([CO2]) was at least double that of the present-day, polar forests populated high latitude landmasses.

We investigated the density and length of stomata and other epidermal cells of two deciduous and three evergreen “living fossil” tree species representative of these ancient forests. These tree species were grown in a simulated Cretaceous high latitude environment at either ambient (400 ppmv) or elevated (800 ppmv) [CO2] during four years.

After 4 years growing at elevated [CO2], the leaf stomatal density and index (percentage of leaf epidermal cells that are stomata) of these plants were similar to those of their counterparts growing at ambient [CO2]. While the CO2 enrichment only modified the stomatal pore length in two of the five studied species, it increased significantly the overall length of the epidermal cells of all the species, reducing their density.

These results revealed that leaf epidermal cells of these “living fossil” species were more sensitive than stomata to an experimental doubling of atmospheric CO2 concentration.

Light intensity, temperature and stomatal morphology

 

 

The effect of light intensity and temperature changes on the stomatal and epidermal morphology of Quercus kelloggi: implications for paleoelevation reconstruction

by Kouwenberg L. L. R., McElwain J. C. (    )

Lenny L.R. Kouwenberg, Jennifer C. McElwain,

http://www.ucmp.berkeley.edu/science/profiles/lenny_poster1.pdf

Introduction

Recently a new method to reconstruct paleoelevation has been developed, based on the adjustment in number of stomata on leaves to the predictable decrease in CO partial pressure with altitude (McElwain, 2004). The first time 2 application of this method focuses on determining the altitude of growth of early Miocene Quercus pseudolyrata leaves from the northern Sierra Nevada. Calibration of the fossil stomatal numbers to altitude is based on the stomatal response of the modern day California black oak (Quercus kelloggi), whose leaves are indistinguishable from Q. pseudolyrata and grows in the same region. The clear correlation between increasing stomatal density and index vs. increasing altitude of growth found in Quercus kelloggii can for a large part be attributed to the predictable decrease in CO partial pressure. Many plants, 2 among which several Quercus species, show this increase in stomatal frequency with decreasing CO and CO is the only environmental parameter that globally and predictably changes with elevation. 2 2 However, several other climatic variables can also change with elevation and potentially influence stomatal density. The most important two are light intensity and temperature. In a natural setting, the relative influence of all environmental parameters on the stomatal change over altitude transect is extremely difficult to pry apart. Therefore, saplings of Quercus kelloggi were grown under controlled conditions in growth chambers, varying the levels of light and temperature. We will present preliminary data on the effect of both light levels and temperature regimes on stomatal frequency and epidermal cell morphology of Quercus kelloggii leaves.

Fossils and the evolution of stomatal function

 

 

Evolution of stomatal function: New perspectives and application to the fossil record

by McElwain J. C. (2012)

JENNIFER C. McELWAIN,

School of Biology and Environmental Science, University College Dublin, Belfield, Dublin, Ireland

==========

Presentation at New Phytologist Symposium Nr. 29 on Stomata 2012 –

https://www.newphytologist.org/app/webroot/img/upload/files/29thNPSAbstractBook.pdf

Abstract

Vascular plants have evolved a suite of different strategies to optimize carbon uptake against water loss via developmental, physiological and cellular level control of stomatal function.

Alterations to the development of stomatal number and size in response to atmospheric CO2 concentration enable some species to regulate stomatal conductance on time-scales of weeks to decades.

Other species demonstrate physiological control of stomatal aperture allowing for rapid control of stomatal function in response to abiotic factors on time scales of seconds to minutes.

Competing hypotheses have been proposed for the evolution of stomatal function in land plants with suggestions on one side that stomatal function is highly conserved across the plant phylogeny and the alternative view that stomatal function has increased incrementally across vascular plants from monilophytes to spermatophytes.

Observations of stomatal response to both instantaneous and long-term exposure to elevated atmospheric CO2 in UCD PÉAC (Programme for Experimental Atmospheres and Climate) do not completely support either competing hypothesis. Rather they suggest that the evolution of stomatal function is more complex and does not display a strong phylogenetic signature.

We show that loss of one aspect of stomatal function in response to an external stimulus can be readily compensated by improved functionality in another.

Experiments also show that there may be a trade-off between physiological control of stomatal conductance via stomatal aperture opening/closing and morphological control of conductance through developmental alteration to stomatal density and pore size.

This “stomatal trade- off hypothesis” is supported by the observation of a significant negative correlation between the magnitude of response of conductance to instantaneous change in CO2 and the magnitude and sign of response of stomatal density to long term elevated CO2 exposure. In other words, species which show rapid instantaneous changes in stomatal conductance do not alter stomatal density inversely under elevated CO2 and vice versa.

This has obvious and important implications for future development and application of the stomatal-CO2 proxy method which uses the inverse relationship between SD and CO2 to reconstruct palaeo-CO2 concentration in the geological past.

This will be discussed in relation to new estimates of palaeo-CO2 spanning the Eocene-Oligocene boundary between 40 and 25 million years ago when the Earth transitioned between an ice-free (greenhouse) and glaciated (icehouse) state.

How land plant life cycles first evolved

Science Magazine
Photo credit: Science – How plant life cycles evolved Plants that lived in the 407-million-year-old Rhynie Chert hot spring system had life cycles that were different from living species.

 

How land plant life cycles first evolved

by Kenrick P. (2017)

Paul Kenrick,

Department of Earth Sciences, The Natural History Museum, London SW7 5BD, UK

 

=========================

in Science 358(6370): 1538-1539 – DOI: 10.1126/science.aan2923 –

http://science.sciencemag.org/content/358/6370/1538.full

This year marks the 100th anniversary of the first in a series of papers on the biota of a 407-million-year-old hot spring system that opened a window onto early life on land (1). The site near the village of Rhynie in Aberdeenshire, Scotland, is exceptional because fossilization occurred in microcrystalline silica (chert), preserving organisms to the cellular level and shedding light on community structure and interactions among the plants, arthropods, fungi, algae, and cyanobacteria. Recent research on these remarkable fossils and advances in understanding plant developmental genetics are beginning to reveal how major changes in life cycle had an early influence on the direction of plant evolution.

When the Rhynie Chert fossils were first reported, the plants, in particular, caused quite a stir because they seemed to capture an early stage in the adaptation to life on land. Most lack key organs familiar in living species, such as leaves or roots. Moreover, they are small (<20 cm), with simple bifurcating axes that terminate in spore-bearing sacs. Later research has revealed that their life cycles also differed in important ways from those of living species.

Land plants inherited their biochemistry and cell biology from ancestral green algae, but their fundamental organs and tissues evolved on land. Their closest algal relatives have a haplontic life cycle, which typically features a simple multicellular haploid sexual phase (a gametophyte) and a unicellular diploid zygote (2). This implies that the ancestor of land plants was also haplontic, probably with a filamentous, weakly differentiated multicellular phase (3).

The transition to land entailed changes in life cycle in which the diploid zygote also became multicellular (4). This change was accompanied by substantial somatic development, resulting in the evolution of tissues and organs basic to plants, such as stems, leaves, roots, a vascular system, stomata (the minute pores that facilitate gaseous exchange), and sex and dispersal organs. The multicellular diploid phase evolved into a highly successful spore-producing dispersal unit (the sporophyte), laying the foundations of modern plant diversity. Changes in life cycle thus underpinned the early diversification of plants on land, but how such changes evolved remains a puzzle.


Life-cycle phases are known in varying degrees of detail for four of the six fossil plant species from the Rhynie Chert. Like ferns, the gametophytes and sporophytes lived as independent plants, but unlike any living land plants, tissues such as rooting structures, a vascular system, and stomata were expressed in both parts of the life cycle (6). Despite these similarities, sporophytes and gametophytes were not identical. Although both were axial and leafless, the gametophytes were smaller. Overall, habit and size are still poorly understood for several gametophytes, but one factor known to influence their size was the degree of development of their branching systems (1). Also, in several species, gametophyte axes terminated in an expanded cup-shaped structure that bore the sexual organs. These differences notwithstanding, the gametophyte bore much greater similarity to the sporophyte than it does in living species, and it developed tissues of greater diversity.

(continued)

Stomatal density and index of a fossil Platanus

 

 

Stomatal density and index data of Platanus neptuni leaf fossils and their evaluation as a CO2 proxy for the Oligocene

by Roth-Nebelsick A., Oehm C., Grein M., Utescher T., Kunzmann L., Friedrich J. P., Konrad W. (2014)

Anita Roth-Nebelsick, a  Christoph Oehm, a  Michaela Grein, b  Torsten Utescher, cd  Lutz Kunzmann, e  Jan-Peter Friedrich, a  Wilfried Konrad, f

a
State Museum of Natural History Stuttgart, Rosenstein 1, D-70191 Stuttgart, Germany
b
Übersee-Museum Bremen, Bahnhofsplatz 13, D-28195 Bremen, Germany
c
Steinmann Institute, Bonn University, Nuβallee 8, D-53115 Bonn, Germany
d
Senckenberg Research Institute, D-60325 Frankfurt, Germany
e
Senckenberg Natural History Collections Dresden, Königsbrücker Landstraβe 159, D-01109 Dresden, Germany
f
University of Tübingen, Department of Geosciences, Hölderlinstrasse 12, D-72074 Tübingen, Germany

==================================

in Rev. Palaeobot. Palynol. – 206: 1– 9 – DOI: 10.1016/j.revpalbo.2014.03.001 –

http://www.sciencedirect.com/science/article/pii/S0034666714000359

Highlights

Stomatal data of Platanus neptuni leaves were used as CO2 proxy for the Oligocene.

CO2 calculation was based on a gas exchange model.

The data indicate quite a constant level of about 400 ppm throughout the Oligocene.

Abstract

Platanus neptuni (Ettingshausen) Bůžek, Holý and Kvaček is a deciduous and preferentially azonal taxon of temperate to warm-temperate vegetation in Europe from the Late Eocene to the Late Miocene. The high fossilization potential of its leaves and easily identifiable stomata and epidermal cells make P. neptuni an excellent source of stomatal data that can be utilized as a CO2proxy. Moreover, it was found in former studies that CO2 data based on stomatal frequency data of P. neptuni overlapped to a high degree with CO2 results which are provided by other, contemporaneous taxa. In this study, the stomatal CO2 signal of P. neptuni is expanded to include the early Oligocene and is analyzed in more detail with three aims: 1) to evaluate the CO2 signal of P. neptuni stomatal data, 2) to check SI and SD data of P. neptuni for consistency, and 3) to contribute additional terrestrial CO2 data to the Oligocene record. During the Oligocene, full scale Antarctic glaciation occurred, punctuated by various distinct glaciation events. There is evidence that Oligocene glaciation was coupled to atmospheric CO2 level. Presently, the main proxy sources for Oligocene CO2 levels are alkenones and boron-isotope data, both obtained from marine sediments.

Since P. neptuni is an extinct taxon, CO2 was reconstructed by using an ecophysiological modeling approach to plant gas exchange which utilizes various other data in addition to stomatal density. Material was considered from sites which are dated to the following time intervals: early Oligocene — 33.9 to 32 Ma, late Oligocene — 27 to 26.2 Ma and 25.3 to 23 Ma, and latest Oligocene — around 24 Ma. Comparison of raw SI and SD data of P. neptuni revealed partially conflicting results, with the SD data indicating a decrease in CO2from the early to the late Oligocene whereas SI data indicate an increase. In contrast, CO2 results calculated with the gas exchange model indicate relatively stable CO2 for the considered time intervals, with levels of about 400 ppm. The reconstructed CO2 data points are similar to other proxy data and are consistent with the general climate development during the Oligocene.