The latitudinal biodiversity gradient through deep time.
Philip D Mannion, Paul Upchurch, Roger B J Benson, Anjali Goswami
January 2014 Trends Ecol EvolSynopsis of Social media discussions
The discussions mainly focus on the clarity of a related video about greenhouse gases and climate change, with some participants highlighting the importance of visual explanations, but few delve into the specifics of the biodiversity gradients presented in the article. The tone is informative but casual, emphasizing accessibility over detailed scientific critique.
Agreement
Neither agree nor disagreeThe discussions show a neutral stance, with some acknowledgment of related topics but no strong alignment or disagreement with the article's findings.
Interest
Moderate level of interestParticipants exhibit mild curiosity, notably engaging more with the climate-related content and visual explanations rather than the scientific details of biodiversity gradients.
Engagement
Neutral engagementComments are brief and primarily share external videos or mentions, indicating surface-level interaction rather than deep analysis.
Impact
Neutral impactThe social discussions seem to reflect general awareness rather than denoting any substantial influence on the audience's understanding of the article.
Social Mentions
YouTube
2 Videos
3 Posts
2 Posts
Blogs
5 Articles
News
15 Articles
Metrics
Video Views
6,147
Total Likes
164
Extended Reach
7,665
Social Features
27
Timeline: Posts about article
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@FoissacPatrice @Azedii1 @Thierry_Lutz @bcassoret @fmbreon Au passage, ce schéma provient de cette vidéo : https://t.co/Tk0lDWqtV8 qui est très claire sur influence des différents GES sur le changement climatique. Très bonne chaîne anglophone de vulgarisation sur le climat.
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Abstract Synopsis
- The current latitudinal biodiversity gradient (LBG), with higher species diversity at the equator than at the poles, is crucial for understanding and predicting climate-related biodiversity loss, but its causes are still not fully understood.
- Fossil records show that this pattern has not always been consistent throughout Earth's history; instead, it has varied over time, appearing mainly during certain periods like the Palaeozoic and the last 30 million years.
- During colder (icehouse) climates, marine biodiversity tends to peak in tropical regions, while warmer (greenhouse) periods often see more evenly distributed or differently peaked diversity patterns across latitudes.]
BRÅTHULT
@BRTHULT1 (Twitter)