{"id":5581,"date":"2019-05-01T15:42:37","date_gmt":"2019-05-01T13:42:37","guid":{"rendered":"https:\/\/www.adssc.org\/en\/?p=5581"},"modified":"2020-07-13T15:08:41","modified_gmt":"2020-07-13T13:08:41","slug":"geodiversity-effects-on-soil-quality-and-geo-ecosystem-functioning-in-drylands","status":"publish","type":"post","link":"https:\/\/www.adssc.org\/en\/geodiversity-effects-on-soil-quality-and-geo-ecosystem-functioning-in-drylands\/","title":{"rendered":"Geodiversity effects on soil quality and geo-ecosystem functioning in drylands"},"content":{"rendered":"<p><u>By<\/u>: <a href=\"https:\/\/www.adssc.org\/en\/reserchers-ilan-stavi-phd\/\" target=\"_blank\" rel=\"noopener noreferrer\">Stavi, I.<\/a>, Rachmilevitch, S., Yizhaq, H.<\/p>\n<p><u>Published in<\/u>: <em>Catena<\/em> 176, 372\u2013380<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0341816219300372\">https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0341816219300372<\/a><\/p>\n<p><u>Correspondence<\/u>: <a href=\"mailto:istavi@adssc.org\">istavi@adssc.org<\/a><\/p>\n<p><strong>Abstract<\/strong><\/p>\n<p data-wp-editing=\"1\">Geodiversity is defined as the natural variability of geologic, geomorphic, and soil features. It has been acknowledged to positively affect biodiversity and species richness. A long-term drought occurring in the semi-arid northern Negev of Israel has led to the mass mortality of shrubs, with the particularly adverse impact on the predominant <em>Noaea mucronata<\/em> species. Recent observations in these shrublands have suggested that this mass mortality is not uniformly distributed over the landscape, but is confined to hillslopes characterized by low-geodiversity. This type of hillslope is defined by a deep (&gt; 1 m) soil layer, lacking rock fragments in its profile, and its surface. Also, the herbaceous vegetation cover of these hillslopes is very high (&gt; 90%), but shrubby vegetation cover is very low (&lt; 10%) and for the most part, non-vital. At the same time, shrubby vegetation in high-geodiversity hillslopes \u2013 defined by a shallow (~ 10 cm) soil layer, and high rock fragment content (&gt; 30% volume) and cover (&gt; 20%) \u2013 is rather dense (&gt; 25%) and vital, but their herbaceous vegetation cover is quite sparse (&lt; 30%). Soil was sampled from the 0\u201310 cm depth in two micro-habitats \u2013 shrubby patches and inter-shrub spaces \u2013 on both the homogeneous and heterogeneous hillslopes. Overall, soil quality was found to be considerably higher in the heterogeneous hillslopes compared to the homogeneous hillslopes. This included the contents of hygroscopic moisture, total organic carbon, particulate organic carbon, and carbon lability, whose means were 22%, 36%, 27%, and 38%, respectively, greater in the heterogeneous hillslopes. Further, mean clay dispersion index was 18% lower in the heterogeneous hillslopes. At the same time, mean soil electrical conductivity was 13% greater in the heterogeneous hillslopes. Yet, this could be attributed to the greater clay content in the former type (19.1%) than that in the latter type (12.7%) of hillslope, with the assumingly higher salt-adsorption from the soil solution. Overall, the results show that the effect of micro-habitat on the soil properties was relatively moderate, and therefore, suggest that the impact of geodiversity might override that of vegetation patchiness. The results highlight the importance of assessing patch-scale and\/or hillslope-scale geodiversity in future studies of dryland ecosystems around the world.<\/p>\n<p><a href=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Stavi-et-al-2019b-Catena_abstract.pdf\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class=\"alignnone size-full wp-image-3804\" src=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2018\/06\/application-pdf.png\" alt=\"\" width=\"16\" height=\"16\" \/>Stavi et al 2019b Catena_abstract<\/a><\/p>\n<figure id=\"attachment_5582\" aria-describedby=\"caption-attachment-5582\" style=\"width: 1523px\" class=\"wp-caption alignnone\"><img fetchpriority=\"high\" decoding=\"async\" class=\"wp-image-5582 size-full\" src=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom.jpg\" alt=\"\" width=\"1523\" height=\"1044\" srcset=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom.jpg 1523w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom-600x411.jpg 600w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom-300x206.jpg 300w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom-1024x702.jpg 1024w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom-768x526.jpg 768w\" sizes=\"(max-width: 1523px) 100vw, 1523px\" \/><figcaption id=\"caption-attachment-5582\" class=\"wp-caption-text\">Fig. 1. a homogeneous hillslope (a); a heterogeneous hillslope (b); a shrubby patch on the homogeneous hillslope (c); a shrubby patch on the heterogeneous hillslope (d).<\/figcaption><\/figure>\n<figure id=\"attachment_5590\" aria-describedby=\"caption-attachment-5590\" style=\"width: 1077px\" class=\"wp-caption alignnone\"><img decoding=\"async\" class=\"wp-image-5590 size-full\" src=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro.jpg\" alt=\"\" width=\"1077\" height=\"1231\" srcset=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro.jpg 1077w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro-600x686.jpg 600w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro-262x300.jpg 262w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro-896x1024.jpg 896w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-2.-Hetro-768x878.jpg 768w\" sizes=\"(max-width: 1077px) 100vw, 1077px\" \/><figcaption id=\"caption-attachment-5590\" class=\"wp-caption-text\">Fig. 2. Schematic illustration of a characteristic pedon-like profile in a homogeneous hillslope (a) and a heterogeneous hillslope (b).<\/figcaption><\/figure>\n<figure id=\"attachment_5589\" aria-describedby=\"caption-attachment-5589\" style=\"width: 910px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-5589 size-full\" src=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes.jpg\" alt=\"\" width=\"910\" height=\"684\" srcset=\"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes.jpg 910w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes-600x451.jpg 600w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes-300x225.jpg 300w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes-768x577.jpg 768w, https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/Ilan_Fig.-3.-Processes-160x120.jpg 160w\" sizes=\"(max-width: 910px) 100vw, 910px\" \/><figcaption id=\"caption-attachment-5589\" class=\"wp-caption-text\">Fig. 3. Feedback loops among the geo-ecosystem components and properties.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>By: Stavi, I., Rachmilevitch, S., Yizhaq, H. Published in: Catena 176, 372\u2013380 https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0341816219300372 Correspondence: istavi@adssc.org Abstract Geodiversity is defined as the natural variability of geologic, geomorphic, and soil features. It has been acknowledged to positively affect biodiversity and species richness. A long-term drought occurring in the semi-arid northern Negev of Israel has led to the [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":5582,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_exactmetrics_skip_tracking":false,"_exactmetrics_sitenote_active":false,"_exactmetrics_sitenote_note":"","_exactmetrics_sitenote_category":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[217],"tags":[],"class_list":{"0":"post-5581","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-new-article"},"jetpack_featured_media_url":"https:\/\/www.adssc.org\/en\/wp-content\/uploads\/2020\/05\/ILAN_Hom.jpg","jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/posts\/5581","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/comments?post=5581"}],"version-history":[{"count":5,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/posts\/5581\/revisions"}],"predecessor-version":[{"id":5863,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/posts\/5581\/revisions\/5863"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/media\/5582"}],"wp:attachment":[{"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/media?parent=5581"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/categories?post=5581"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.adssc.org\/en\/wp-json\/wp\/v2\/tags?post=5581"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}