Example of Polar Biology format
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Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format
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Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format Example of Polar Biology format
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open access Open Access

Polar Biology — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Agricultural and Biological Sciences (all) #40 of 209 down down by 5 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 775 Published Papers | 2814 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 14/07/2020
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Springer

Quality:  
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CiteRatio: 6.1
SJR: 1.127
SNIP: 1.528

Journal Performance & Insights

Impact Factor

CiteRatio

Determines the importance of a journal by taking a measure of frequency with which the average article in a journal has been cited in a particular year.

A measure of average citations received per peer-reviewed paper published in the journal.

1.728

14% from 2018

Impact factor for Polar Biology from 2016 - 2019
Year Value
2019 1.728
2018 2.002
2017 1.954
2016 1.949
graph view Graph view
table view Table view

3.6

CiteRatio for Polar Biology from 2016 - 2020
Year Value
2020 3.6
2019 3.6
2018 3.4
2017 3.2
2016 3.1
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 14% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • This journal’s CiteRatio is in the top 10 percentile category.

SCImago Journal Rank (SJR)

Source Normalized Impact per Paper (SNIP)

Measures weighted citations received by the journal. Citation weighting depends on the categories and prestige of the citing journal.

Measures actual citations received relative to citations expected for the journal's category.

0.874

2% from 2019

SJR for Polar Biology from 2016 - 2020
Year Value
2020 0.874
2019 0.861
2018 0.899
2017 0.967
2016 0.915
graph view Graph view
table view Table view

0.885

4% from 2019

SNIP for Polar Biology from 2016 - 2020
Year Value
2020 0.885
2019 0.854
2018 0.903
2017 0.916
2016 0.788
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has increased by 2% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 4% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Polar Biology

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Springer

Polar Biology

Polar Biology publishes Original Papers, Reviews, and Short Notes and is the focal point for biologists working in polar regions. It is also of interest to scientists working in biology in general, ecology and physiology, as well as in oceanography and climatology related to p...... Read More

Agricultural and Biological Sciences

i
Last updated on
14 Jul 2020
i
ISSN
0722-4060
i
Impact Factor
Medium - 0.988
i
Open Access
Yes
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
i
Bibliography Name
SPBASIC
i
Citation Type
Author Year
(Blonder et al, 1982)
i
Bibliography Example
Beenakker CWJ (2006) Specular andreev reflection in graphene. Phys Rev Lett 97(6):067,007, URL 10.1103/PhysRevLett.97.067007

Top papers written in this journal

Journal Article DOI: 10.1007/BF00243114
Ecology of sea ice biota 2. Global significance.
01 Sep 1992 - Polar Biology

Abstract:

The sea ice does not only determine the ecology of ice biota, but it also influences the pelagic systems under the ice cover and at ice edges. In this paper, new estimates of Arctic and Antarctic production of biogenic carbon are derived, and differences as well as similarities between the two oceans are examined. In ice-cove... The sea ice does not only determine the ecology of ice biota, but it also influences the pelagic systems under the ice cover and at ice edges. In this paper, new estimates of Arctic and Antarctic production of biogenic carbon are derived, and differences as well as similarities between the two oceans are examined. In ice-covered seas, high algal concentrations (blooms) occur in association with several types of conditions. Blooms often lead to high sedimentation of intact cells and faecal pellets. In addition to ice-related blooms, there is progressive accumulation of organic matter in Arctic multi-year ice, whose fate may potentially be similar to that of blooms. A fraction of the carbon fixed by microalgae that grow in sea ice or in relation to it is exported out of the production zone. This includes particulate material sinking out of the euphotic zone, and also material passed on to the food web. Pathways through which ice algal production does reach various components of the pelagic and benthic food webs, and through them such top predators as marine mammals and birds, are discussed. Concerning global climate change and biogeochemical fluxes of carbon, not all export pathways from the euphotic zone result in the sequestration of carbon for periods of hundreds of years or more. This is because various processes, that take place in both the ice and the water column, contribute to mineralize organic carbon into CO2 before it becomes sequestered. Processes that favour the production and accumulation of biogenic carbon as well as its export to deep waters and sequestration are discussed, together with those that influence mineralization in the upper ice-covered ocean. read more read less

Topics:

Sea ice (69%)69% related to the paper, Lead (sea ice) (64%)64% related to the paper, Photic zone (56%)56% related to the paper, Arctic (54%)54% related to the paper, Global warming (54%)54% related to the paper
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498 Citations
Journal Article DOI: 10.1007/S00300-004-0667-4
The nature of the diversity of Antarctic fishes
Joseph T. Eastman1
01 Jan 2005 - Polar Biology

Abstract:

The species diversity of the Antarctic fish fauna changed notably during the ≈40 million years from the Eocene to the present. A taxonomically restricted and endemic modern fauna succeeded a taxonomically diverse and cosmopolitan Eocene fauna. Although the Southern Ocean is 10% of the world’s ocean, its current fish fauna con... The species diversity of the Antarctic fish fauna changed notably during the ≈40 million years from the Eocene to the present. A taxonomically restricted and endemic modern fauna succeeded a taxonomically diverse and cosmopolitan Eocene fauna. Although the Southern Ocean is 10% of the world’s ocean, its current fish fauna consists of only 322 species, small considering the global diversity of ≈25,000–28,000 species. The fauna is “reasonably well-known” from a taxonomic perspective. This intermediate designation between “poorly known” and “well-known” indicates that new species are regularly being described. A conservative estimate of the number of undescribed species is ≈30–60; many of these may be liparids. On the Antarctic continental shelf and upper slope the fauna includes 222 species from 19 families of benthic fishes. The most speciose taxa are notothenioids, liparids and zoarcids, accounting for 88% of species diversity. Endemism for Antarctic species is also, coincidentally, 88%, at least threefold higher than in faunas from other isolated marine localities. Eight notothenioid families, including five that are primarily Antarctic, encompass a total of 44 genera and 129 species, 101 Antarctic and 28 non-Antarctic. The 101 Antarctic species make up 45% of the benthic species diversity in the Antarctic region. However, at the highest latitudes, notothenioids contribute 77% of the species diversity, 92% of the abundance and 91% of the biomass. Although species diversity is low compared to other shelf habitats, the nature of the adaptive radiation in organismal diversity among notothenioids is noteworthy in the marine realm. In some notothenioid clades phyletic diversification was accompanied by considerable morphological and ecological diversification. The exemplar is the benthic family Nototheniidae that underwent a habitat or depth related diversification centred on the alteration of buoyancy. They occupy an array of pelagic and benthopelagic habitats at various depths on the shelf and upper slope. Diversification in buoyancy is the hallmark of the nototheniid radiation and, in the absence of swim bladders, was accomplished by a combination of reduced skeletal mineralisation and lipid deposition. Although neutral buoyancy is found in only five species of nototheniids some, like Pleuragramma antarcticum, are abundant and ecologically important. Much work remains to be done in order to frame and to use phylogenetically based statistical methods to test hypotheses relating to the key features of the notothenioid radiation. To reach this analytical phase more completely resolved cladograms that include phyletically basal and non-Antarctic species are essential. read more read less

Topics:

Species diversity (62%)62% related to the paper, Fauna (56%)56% related to the paper, Notothenioidei (56%)56% related to the paper, Endemism (54%)54% related to the paper, Biodiversity (53%)53% related to the paper
369 Citations
Book Chapter DOI: 10.1007/978-3-642-77595-6_17
Dynamics of nutrients and phytoplankton, and fluxes of carbon, nitrogen and silicon in the Antarctic Ocean
Paul Tréguer1, Guy Jacques
01 Sep 1992 - Polar Biology

Abstract:

Four major functional units have been identified in the Southern Ocean and the mechanisms that control the dynamics of nutrients and phytoplankton are detailed for the different sub-systems. The very productive Coastal and Continental Shelf Zone (CCSZ, 0.9 M km 2) can experience severe macronutrient depletion paralleling inte... Four major functional units have been identified in the Southern Ocean and the mechanisms that control the dynamics of nutrients and phytoplankton are detailed for the different sub-systems. The very productive Coastal and Continental Shelf Zone (CCSZ, 0.9 M km 2) can experience severe macronutrient depletion paralleling intense diatom-dominated phytoplankton blooming (maximum > 8 mg Chl a m−3) at the ice edge. In the Seasonal Ice Zone (SIZ, 16 M km 2) dramatic variations in the hydrological structure occur in surface waters during the spring to summer retreat of the pack-ice, changing from a well-mixed system to a stratified one within the reaches of the ice edge. Grazing activity of euphausiids limits phytoplankton biomass to a moderate level (Chl a maximum around 4mg m−3). A shift from new production to a regenerated production regime has been demonstrated during spring, along with the key role played by protozoans in controlling high ammonium concentrations (maximum > 2 μM) in the surface layers. The well-mixed Permanently Open Ocean Zone (POOZ, 14 M km 2) is characterised by variable N/Si ratios in surface waters along a north-south transect: at the northern border of the POOZ (N/Si = 0.25) silicate concentrations as low as <10 μM could help limit the phytoplankton growth. Although favourable conditions have been demonstrated for the initiation of blooms in spring in the Antarctic Circumpolar Current, it appears that critical-depth/ mixing-depth relationships control maximum chlorophyll a concentrations < 1 μg l−1 during summer. The POOZ is usually not influenced directly by euphausiids, except for the Scotia Sea and Drake Passage where migrations of krill from the adjacent SIZ are usual. Mesoscale eddies are typical of the Polar Front Zone (FPZ, 3 M km 2): significant increases in phytoplankton biomass have been reported in this frontal area (maximum Chl a = 2 mg m−3). Food web and biogeochemical cycles in this sub-system are poorly documented. The question of limitation of the primary production by eolian-transported trace-metals in these different sub-systems is still a matter of debate, although clear iron limitation has been evidenced for offshore waters of the Ross Sea. read more read less

Topics:

Phytoplankton (55%)55% related to the paper, New production (54%)54% related to the paper, Krill (51%)51% related to the paper, Polar front (51%)51% related to the paper, Biogenic silica (50%)50% related to the paper
340 Citations
Journal Article DOI: 10.1007/BF00237945
Increases in Antarctic penguin populations: reduced competition with whales or a loss of sea ice due to environmental warming?
William R. Fraser1, Wayne Z. Trivelpiece1, David G. Ainley1, Susan G. Trivelpiece1
01 Mar 1992 - Polar Biology

Abstract:

A central tenet of Antarctic ecology suggests that increases in Chinstrap Penguin (Pygoscelis antarctica) populations during the last four decades resulted from an increase in prey availability brought on by the decrease in baleen whale stocks. We question this tenet and present evidence to support the hypothesis that these i... A central tenet of Antarctic ecology suggests that increases in Chinstrap Penguin (Pygoscelis antarctica) populations during the last four decades resulted from an increase in prey availability brought on by the decrease in baleen whale stocks. We question this tenet and present evidence to support the hypothesis that these increases are due to a gradual decrease in the frequency of cold years with extensive winter sea ice cover resulting from environmental warming. Supporting data were derived from one of the first, major multidisciplinary winter expedition to the Scotia and Weddell seas; recent satellite images of ocean ice cover; and the analysis of long-term surface temperature records and penguin demography. Our observations indicate there is a need to pay close attention to environmental data in the management of Southern Ocean resources given the complexity of relating biological changes to ecological perturbations. read more read less

Topics:

Sea ice (59%)59% related to the paper, Baleen whale (53%)53% related to the paper
313 Citations
Book Chapter DOI: 10.1007/978-3-642-59419-9_21
On the direct impact of ice on marine benthic communities, a review
Julian Gutt1
01 Aug 2001 - Polar Biology

Abstract:

Ice has a significant impact on the polar and sub-polar benthos, but relationships between corresponding physical and biological processes are not yet sufficiently understood. Sea ice contributes to a vertical zonation in shallow waters, which also experience other important disturbances. Due to the length of the non-glaciate... Ice has a significant impact on the polar and sub-polar benthos, but relationships between corresponding physical and biological processes are not yet sufficiently understood. Sea ice contributes to a vertical zonation in shallow waters, which also experience other important disturbances. Due to the length of the non-glaciated coastline, sea ice is of greater relevance in the north than in the south. Scouring by icebergs and ridged sea ice causes an increased diversity when different recolonisation stages coexist. Frequently scoured areas do not recover, especially in the Antarctic, due to slow growth rates of the fauna. Iceberg grounding in the Arctic is mainly restricted to the western Eurasian and northeastern American shelf, including Greenland. Around Antarctica, scouring is more evenly distributed. Glacier termini prevent sessile animals from settling in their proximity where only few motile species occur. read more read less

Topics:

Sea ice (69%)69% related to the paper, Antarctic sea ice (69%)69% related to the paper, Ice shelf (68%)68% related to the paper, Arctic ice pack (68%)68% related to the paper, Fast ice (68%)68% related to the paper
306 Citations
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With SciSpace, you do not need a word template for Polar Biology.

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You can download a submission ready research paper in pdf, LaTeX and docx formats.

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Polar Biology format uses SPBASIC citation style.

Automatically format and order your citations and bibliography in a click.

SciSpace allows imports from all reference managers like Mendeley, Zotero, Endnote, Google Scholar etc.

Frequently asked questions

1. Can I write Polar Biology in LaTeX?

Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the Polar Biology guidelines and auto format it.

2. Do you follow the Polar Biology guidelines?

Yes, the template is compliant with the Polar Biology guidelines. Our experts at SciSpace ensure that. If there are any changes to the journal's guidelines, we'll change our algorithm accordingly.

3. Can I cite my article in multiple styles in Polar Biology?

Of course! We support all the top citation styles, such as APA style, MLA style, Vancouver style, Harvard style, and Chicago style. For example, when you write your paper and hit autoformat, our system will automatically update your article as per the Polar Biology citation style.

4. Can I use the Polar Biology templates for free?

Sign up for our free trial, and you'll be able to use all our features for seven days. You'll see how helpful they are and how inexpensive they are compared to other options, Especially for Polar Biology.

5. Can I use a manuscript in Polar Biology that I have written in MS Word?

Yes. You can choose the right template, copy-paste the contents from the word document, and click on auto-format. Once you're done, you'll have a publish-ready paper Polar Biology that you can download at the end.

6. How long does it usually take you to format my papers in Polar Biology?

It only takes a matter of seconds to edit your manuscript. Besides that, our intuitive editor saves you from writing and formatting it in Polar Biology.

7. Where can I find the template for the Polar Biology?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Polar Biology's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

8. Can I reformat my paper to fit the Polar Biology's guidelines?

Of course! You can do this using our intuitive editor. It's very easy. If you need help, our support team is always ready to assist you.

9. Polar Biology an online tool or is there a desktop version?

SciSpace's Polar Biology is currently available as an online tool. We're developing a desktop version, too. You can request (or upvote) any features that you think would be helpful for you and other researchers in the "feature request" section of your account once you've signed up with us.

10. I cannot find my template in your gallery. Can you create it for me like Polar Biology?

Sure. You can request any template and we'll have it setup within a few days. You can find the request box in Journal Gallery on the right side bar under the heading, "Couldn't find the format you were looking for like Polar Biology?”

11. What is the output that I would get after using Polar Biology?

After writing your paper autoformatting in Polar Biology, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Polar Biology's impact factor high enough that I should try publishing my article there?

To be honest, the answer is no. The impact factor is one of the many elements that determine the quality of a journal. Few of these factors include review board, rejection rates, frequency of inclusion in indexes, and Eigenfactor. You need to assess all these factors before you make your final call.

13. What is Sherpa RoMEO Archiving Policy for Polar Biology?

SHERPA/RoMEO Database

We extracted this data from Sherpa Romeo to help researchers understand the access level of this journal in accordance with the Sherpa Romeo Archiving Policy for Polar Biology. The table below indicates the level of access a journal has as per Sherpa Romeo's archiving policy.

RoMEO Colour Archiving policy
Green Can archive pre-print and post-print or publisher's version/PDF
Blue Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
Yellow Can archive pre-print (ie pre-refereeing)
White Archiving not formally supported
FYI:
  1. Pre-prints as being the version of the paper before peer review and
  2. Post-prints as being the version of the paper after peer-review, with revisions having been made.

14. What are the most common citation types In Polar Biology?

The 5 most common citation types in order of usage for Polar Biology are:.

S. No. Citation Style Type
1. Author Year
2. Numbered
3. Numbered (Superscripted)
4. Author Year (Cited Pages)
5. Footnote

15. How do I submit my article to the Polar Biology?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Polar Biology's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Polar Biology in Endnote format?

Yes, SciSpace provides this functionality. After signing up, you would need to import your existing references from Word or Bib file to SciSpace. Then SciSpace would allow you to download your references in Polar Biology Endnote style according to Elsevier guidelines.

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I spent hours with MS word for reformatting. It was frustrating - plain and simple. With SciSpace, I can draft my manuscripts and once it is finished I can just submit. In case, I have to submit to another journal it is really just a button click instead of an afternoon of reformatting.

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